Updated on 2024/11/16

写真a

 
MATTA Nobuhisa
 
Organization
Faculty of Education Professor
Position
Professor
Contact information
メールアドレス
External link

Degree

  • PhD ( 2002.9   The University of Tokyo )

Research Interests

  • physical geography

  • natural hazard

  • tectonic geomorphology, active fault

Research Areas

  • Natural Science / Human geosciences  / 防災の地理学

  • Natural Science / Solid earth sciences  / テクトニクス

  • Humanities & Social Sciences / Geography  / 変動地形学

Education

  • The University of Tokyo   大学院理学系研究科   地球惑星科学専攻

    1999.4 - 2002.9

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  • The University of Tokyo   大学院理学系研究科   地理学専攻

    1997.4 - 1999.3

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  • The University of Tokyo   理学部   地学科地理学専攻

    1994.4 - 1997.3

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  • The University of Tokyo   理科Ⅱ類  

    1992.4 - 1994.3

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Research History

  • Okayama University   Graduate School of Education   Professor

    2017.4

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  • Nagoya University   Graduate School of Environmental Studies

    2017.4

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  • 東濃地震科学研究所   研究員

    2014.4 - 2020.3

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  • Okayama University   Graduate School of Education   Associate Professor

    2014.4 - 2017.3

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  • Nagoya University   環境学研究科

    2014.4 - 2017.3

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  • Nagoya University   Disaster Mitigation Research Center

    2012.4 - 2014.3

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  • Nagoya University   Graduate School of Environmental Studies Research Center for Seismology, Volcanology and Disaster Mitigation

    2010.1 - 2012.3

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  • National Taiwan Univ.   理学院地質科学系

    2005.3 - 2009.12

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    Country：Taiwan, Province of China

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  • CSIS

    2004.4

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  • ASSOCIATION FOR THE DEVELOPMENT OF EARTHQUAKE PREDICTION

    2004.4 - 2005.3

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  • ERI

    2002.10 - 2004.3

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Professional Memberships

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Committee Memberships

  • 地域地理科学会   編集委員長  

    2022.6   

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    Committee type：Academic society

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  • The Japanese Society for Active Fault Studies   board member  

    2022.4   

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    Committee type：Academic society

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  • 岡山市消防局   住宅火災における避難に関する検討会  

    2021.4 - 2023.3   

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  • Japan Geoscience Union   General Affairs Committee  

    2020.4   

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    Committee type：Academic society

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  • the Association of Japanese Geographers   representative  

    2020.4   

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    Committee type：Academic society

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  • 美咲町教育委員会   美咲町柵原地域学校建設用地検討委員会委員長  

    2019.11 - 2019.12   

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    Committee type：Municipal

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  • Japan Association for Quaternary Research   member of editorial board  

    2018.7 - 2023.6   

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    Committee type：Academic society

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  • 岡山県土木部   岡山県公有水面埋立協議会  

    2017.4   

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    Committee type：Municipal

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  • 岡山県土木部   岡山県河川整備検討委員会  

    2015.4   

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    Committee type：Municipal

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  • 国土地理院   全国活断層帯情報整備検討委員会  

    2010.4   

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    Committee type：Government

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  • THE SOCIETY FOR SYSTEMATIC REGIONAL GEOGRAPHY   executive  

       

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    Committee type：Academic society

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Papers

  • Coastal changes associated with the 2024 Noto Peninsula Earthquake

    Ken-ichi Yasue, Ryo Tateishi, Tatsuya Ishiyama, Nobuhisa Matta, Daisuke Hirouchi, Yoshiki Shirahama

    The Quaternary Research (Daiyonki-Kenkyu)   63 ( 2 )   viii - x   2024.5

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    Publishing type：Research paper (scientific journal)   Publisher：Japan Association for Quaternary Research  

    DOI： 10.4116/jaqua.63.2410i

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  • The study of applicability of the very shallow geophysical exploration method for the strike-slip fault (part 2; S-wave shallow seismic reflection survey and two-dimensional electrical resistivity survey): the case study of the Go-mura fault zone and Yamada fault zone

    Sakashita Susumu, Okada Shinsuke, Imai Mikio, Imaizumi Toshifumi, Okada Atsumasa, Nakamura Norihiro, Fukuchi Tatsuro, Kagohara Kyoko, Jomori Akira, Toda Shigeru, Matta Nobuhisa, Yamaguchi Satoru, Matsubara Yoshikazu, Yamamoto Masato, Todokoro Hitoshi

    BUTSURI-TANSA(Geophysical Exploration)   75   1 - 20   2022

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    Language：Japanese   Publisher：The Society of Exploration Geophysicists of Japan  

    S-wave shallow seismic reflection survey and two-dimensional electrical resistivity survey targeting depths less than 100 m were applied to the strike-slip fault. This study was conducted in the Go-mura fault zone and the Yamada fault zone where surface rupture occurred during the 1927 Kita Tango earthquake. For the interpretation of the two-dimensional electrical resistivity survey results, we carried out in situ measurement of the electrical resistivity on outcrops around the survey area. It was confirmed that there is 10 times contrast in the electrical resistivity between the fresh or weathering granite and the fracturing part or clay part of granite. At the study area in the Go-mura fault zone, discontinuity and deformation of the reflection surface from the S-wave shallow seismic reflection profile corresponds to the location and displacement sense of the active fault estimated by boring and trench survey. As the result of applying two-dimensional electrical resistivity survey, the low resistivity zone continuing from deep underground to shallow was recognized near the active fault trace on the ground. This low resistivity zone indicates the fracture zone of host rock with fluid supply from fault activity. At the study area in the Yamada fault zone, the similar survey results as in the study area of the Go-mura fault zone were obtained. Discontinuity and deformation of the reflection surface from the S-wave shallow seismic reflection profile corresponds to the location and displacement sense of the active fault. In addition, as the result of two-dimensional electrical resistivity survey, the low resistivity zone continuing from deep underground to shallow was recognized near the active fault trace on the ground. The low resistivity zone was confirmed to be continuous down to the depth of 300 m or deeper by comparing with CSAMT survey result. Two-dimensional electrical resistivity survey was carried out with multiple measurement lines at another study area where the stepping of the active fault trace on the ground has been inferred from the comparison of the strike of the Yamada fault zone. As a result, the low resistivity zone was distributed almost linearly underground, and it could be shown that the distribution of active faults might be different between the surface and the underground.

    DOI： 10.3124/segj.75.1

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  • Surface Ruptures Accompanied with the Largest Foreshock

    Nobuhiko Sugito, Hideaki Goto, Yasuhiro Kumahara, Hiroyuki Tsutsumi, Takashi Nakata, Kyoko Kagohara, Nobuhisa Matta, Mitsuhisa Watanabe

    Surface Ruptures Associated with the 2016 Kumamoto Earthquake Sequence in Southwest Japan   233 - 241   2022

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    Publishing type：Part of collection (book)   Publisher：Springer Nature Singapore  

    DOI： 10.1007/978-981-19-1150-7_18

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  • Surface Ruptures of the Shirahata–Oike Section

    Yasuhiro Kumahara, Tatsuya Ishiyama, Nobuhisa Matta, Kyoko Kagohara, Daisuke Hirouchi, Satoshi Ishiguro

    Surface Ruptures Associated with the 2016 Kumamoto Earthquake Sequence in Southwest Japan   37 - 46   2022

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    Publishing type：Part of collection (book)   Publisher：Springer Nature Singapore  

    DOI： 10.1007/978-981-19-1150-7_7

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  • Faulting event of the Northern part of Kamishiro fault, ISTL active fault zone, central Japan Reviewed

    hirouchi daisuke, shiono toshiaki, Matsuta nobuhisa, yasue kenichi, takeshita yoshihiro, doke ryosuke, sato yoshiki, ishimura daisuke, ishiyama tatsuya, sugito nobuhiko

    Proceedings of the General Meeting of the Association of Japanese Geographers   2017 ( 0 )   100281 - 100281   2017

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    Language：Japanese   Publisher：The Association of Japanese Geographers  

    DOI： 10.14866/ajg.2017s.0_100281

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  • Surface fault ruptures associated with the 14 April foreshock (Mj 6.5) of the 2016 Kumamoto earthquake sequence, southwest Japan

    Nobuhiko Sugito, Hideaki Goto, Yasuhiro Kumahara, Hiroyuki Tsutsumi, Takashi Nakata, Kyoko Kagohara, Nobuhisa Matsuta, Haruka Yoshida

    Earth, Planets and Space   68 ( 1 )   2016.12

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    The 2016 Kumamoto earthquake sequence was a rare event worldwide in that the surface ruptures associated with the largest foreshock (Mj 6.5) of 21:26 (JST), 14 April ruptured again during the mainshock (Mj 7.3) of 01:25 (JST), 16 April. The 14 April Mj 6.5 earthquake produced 6-km-long surface ruptures along the central portion of the Futagawa-Hinagu fault zone (FHFZ). The mainshock produced 31-km-long surface ruptures along the central to northeastern part of the FHFZ. Field observations and eyewitness accounts documented that the offsets of the ruptures associated with the 14 April foreshock became larger after the 16 April mainshock, suggesting that the same portion of the fault ruptured to the surface twice in the Kumamoto earthquake sequence. The 6-km-long surface ruptures associated with the largest foreshock are located near a geometric bend of the FHFZ characterized by ~50° change in strike. The epicenter of the mainshock is also located near the bend. These observations imply that the Kumamoto earthquake sequence was initiated due to a stress concentration on the bend of the FHFZ, and the mainshock was initiated approximately at the same place about 28 h after the largest foreshock. This foreshock/mainshock sequence of the Kumamoto earthquake is not successive events on the adjacent different fault zones, because the 6-km-long surface ruptures of the largest foreshock are part of the 31-km-long surface ruptures of the mainshock.[Figure not available: see fulltext.].

    DOI： 10.1186/s40623-016-0547-5

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  • Application of terrestrial laser scanning for detection of ground surface deformation in small mud volcano (Murono, Japan) Reviewed

    Yuichi S. Hayakawa, Shigekazu Kusumoto, Nobuhisa Matta

    Earth, Planets and Space   68 ( 1 )   2016.7

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    Language：English   Publishing type：Research paper (scientific journal)   Publisher：Springer Nature  

    We perform terrestrial laser scanning (TLS) to detect changes in surface morphology of a mud volcano in Murono, north-central Japan. The study site underwent significant deformation by a strong earthquake in 2011, and the surface deformation has continued in the following years. The point cloud datasets were obtained by TLS at three different times in 2011, 2013 and 2014. Those point clouds were aligned by cloud-based registration, which minimizes the closest point distance of point clouds of unchanged ground features, and the TLS-based point cloud data appear to be suitable for detecting centimeter-order deformations in the central domain of the mud volcano, as well as for measurements of topographic features including cracks of paved ground surface. The spatial patterns and accumulative amount of the vertical deformation during 2011-2014 captured by TLS correspond well with those previously reported based on point-based leveling surveys, supporting the validity of TLS survey.

    DOI： 10.1186/s40623-016-0495-0

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  • Understanding Spatial Variations of Tsunami Flooding

    N. Sugito, Yoshitsugu Suzuki, N. Matsuta

    Disaster Resilient Cities: Concepts and Practical Examples   75 - 83   2016.3

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    This chapter examines damage maps produced at the time of a large-scale disaster and their roles. Materials for examination are our tsunami inundation area map prepared using posttsunami aerial photographs, and mapping results of the tsunami run-up heights measured using a digital elevation model afterward. Based on these examinations, we reveal the remarkable spatial variation in the range and height inundated by the tsunami, and discuss its scientific significance and lessons for disaster management.

    DOI： 10.1016/B978-0-12-809862-2.00003-6

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  • Holocene uplifted coral reefs in Lanyu and Lutao Islands to the southeast of Taiwan

    S. Inoue, H. Kayanne, N. Matta, W. S. Chen, Y. Ikeda

    Coral Reefs   30 ( 3 )   581 - 592   2011.9

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    Lanyu and Lutao Islands to the southeast of Taiwan are located in the northern extension of the Luzon Arc. Crustal deformation of these islands provides a key to understand the collision of the Luzon Arc against Taiwan. To clarify the style and the rate of vertical movement during the Holocene, uplifted coral reefs fringing these two islands were investigated. Living corals were also investigated for comparison with fossil corals. It was found that Isopora palifera lives dominantly in the upper slope of the present-day fringing coral reefs in Lanyu Island at an average depth of 101 ± 46 cm (one standard deviation) below mean sea level. Using I. palifera as an accurate indicator of paleo-sea levels, Holocene relative sea-level changes were reconstructed. Lanyu Island has been uplifted continuously at a rate of 2. 0 mm yr -1, at least during the late Holocene from 2,269 cal. yr BP to the present. Lutao Island has been uplifted at an average rate of 1. 2 mm yr -1, since at least 5,749 cal. yr BP, although it is unclear whether the uplift was continuous. The present observations, combined with the GPS displacement field and deep crustal structure, suggest that the continuous uplift is related to aseismic slip on the Longitudinal Valley Fault. © 2011 Springer-Verlag.

    DOI： 10.1007/s00338-011-0783-x

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  • The 1999 Earthquake Fault and Its Repeated Occurrence at the Earthquake Museum, Central Part of Chelungpu Fault, Taiwan

    Yoko Ota, Nobuhisa Matta

    TERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES   21 ( 4 )   737 - 741   2010.8

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    Language：English   Publishing type：Research paper (scientific journal)   Publisher：CHINESE GEOSCIENCE UNION  

    This paper reports on the trench log data covering the Chelungpu Fault preserved at the National Science Museum and 10 bore hole data across the fault. Trench log indicates the vertical offset of the 1999 displacement of terrace deposits is ca. 1.5 m and the presence of four branch faults cutting terrace deposits within 1.8 m width zone. Estimated height difference of bedrock surface based on bore hole data is more than 4.2 - 5.8 m, larger than the offset by the 1999 earthquake. These facts imply that at least one earthquake event occurred at this site before the 1999 earthquake. We also estimate the fault plane dips eastward at about 30 degrees based on the location and stratigraphy of one bore hole which penetrates the terrace gravel on the hanging wall through the bedrock.

    DOI： 10.3319/TAO.2009.08.25.02(TT)

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  • Touhuanping Fault, an active wrench fault within fold-and-thrust belt in northwestern Taiwan, documented by spatial analysis of fluvial terraces

    Yoko Ota, Yu Nung Nina Lin, Yue Gau Chen, Nobuhisa Matsuta, Takuya Watanuki, Ya Wen Chen

    Tectonophysics   474 ( 3-4 )   559 - 570   2009.9

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    This study aims at the recent activity and development of an active wrench fault, the Touhuanping Fault in northwestern Taiwan. Northwestern Taiwan has been proposed in a current situation between the mature to waning collision in terms of tectonic evolution. The main drainage in this area, the Chungkang River, flows close to the trace of the fault mentioned above. We examined various types of deformation of fluvial terraces along the Chungkang River as a key to understanding the nature and rate of the late Quaternary tectonics. The E-W trending Touhuanping Fault has long been mapped as a geological boundary fault, but its recent activity was suspected. Field survey revealed that its late Quaternary activity is recorded in the offset fluvial terraces. Our result shows dextral slip and vertical offset with upthrown side on the south, and activated at least twice since the emergence of terrace 4 (older terrace 3 with OSL date of ca. 80 ka). Total amount of offset recorded in the Touhuanping terrace sequence is 15 m for dextral and 10 m for vertical offset. Estimated recurrence time of earthquake rupture may be a few tens of thousand years. Uplift on the upthrown side of the Touhuanping Fault also resulted in the formation of drowned valleys which were graded to terrace 4. Other deformation features, such as back-tilting, westward warping, and a range-facing straight scarp, were also identified. A second-order anticline roughly parallel to the Touhuanping Fault is suggested to be the origin of the northward tilting on terrace 3; it could have resulted from a flower structure on the Touhuanping Fault at shallow depth. This may demonstrate that the buried segment of the Touhuanping Fault has also been active since 80 ka. In the northern study area, the westward warping at terrace 2 probably represents late Quaternary activity of another NE-SW trending Hsincheng Fault. © 2009 Elsevier B.V. All rights reserved.

    DOI： 10.1016/j.tecto.2009.04.034

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  • Subsurface geometry and structural evolution of the eastern margin fault zone of the Yokote basin based on seismic reflection data, northeast Japan

    Kyoko Kagohara, Tatsuya Ishiyama, Toshifumi Imaizumi, Takahiro Miyauchi, Hiroshi Sato, Nobuhisa Matsuta, Atsushi Miwa, Takeshi Ikawa

    Tectonophysics   470 ( 3-4 )   319 - 328   2009.5

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    High-resolution seismic reflection profiles across coseismic fault scarps reactivated during the A.D. 1896 Rikuu earthquake along the eastern margin fault zone of the Yokote basin (EFZYB) in northeast Japan, correlated with borehole stratigraphy and geologic mapping, provide insights into its detailed kinematic history and structural evolution. In spite of along-strike variations of thrust geometries both at ground surface and at shallow depth, the EFZYB has commonly formed as forward breaking imbricate thrust systems. Near surface complexity of thrust geometries appears strongly affected by mechanical decoupling between layers within middle to late Miocene mudstone. Cross-section balancing across the Mahiru Mountains shows strong correlation of the millennial uplift rates with mountain topography but its weak correlation with the late Pleistocene uplift rates. Considering the thrust trajectories estimated by the balanced cross sections, the millennial dip-slip rate are consistent with the late Pleistocene dip-slip rate, suggesting that the EFZYB has accumulated strains at a constant rate since the onset of its fault activity. © 2009 Elsevier B.V. All rights reserved.

    DOI： 10.1016/j.tecto.2009.02.007

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  • Crustal structure in the northern Fossa Magna region, central Japan, modeled from refraction/wide-angle reflection data

    Tetsuya Takeda, Hiroshi Sato, Takaya Iwasaki, Nobuhisa Matsuta, Shin'ichi Sakai, Takashi Iidaka, Aitaro Kato

    Earth, Planets and Space   56 ( 12 )   1293 - 1299   2004.12

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    The northern Fossa Magna (NFM) is a back-arc rift basin filled with thick Tertiary sediments, which show strong NW-SE shortening deformation. In the NFM, there exist two major active fault systems, the Itoigawa-Shizuoka Tectonic Line active fault system (ISTL) and the Western Nagano Basin active fault system (WNB), both of which have great potentials to cause destructive earthquakes. By reanalyzing five sets of refraction/wide-angle reflection data, we successfully obtained detailed and consistent models of the crustal structure in the NFM region. It was a very effective modeling procedure to incorporate vicinal seismic reflection data and geologic information. The geometries of the active faults in the NFM region were revealed. The ISTL is east dipping, and the WNB is northwest dipping. The Tertiary sedimentary layer (<4.0 km/sec) west and adjacent to the ISTL extends to a depth of 4-5 km. The basement rocks below the Central Uplift Belt (CUB) form a wedge structure, which suggests the westward movement of the CUB basement rocks. © 2004, The Seismological Society of Japan, Society of Geomagnetism and Earth, Planetary and Space Sciences, The Volcanological Society of Japan, The Geodetic Society of Japan, The Japanese Society for Planetary Sciences. All rights reserved.

    DOI： 10.1186/BF03353353

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  • Formation and shortening deformation of a back-arc rift basin revealed by deep seismic profiling, central Japan

    Hiroshi Sato, Takaya Iwasaki, Shinji Kawasaki, Yasutaka Ikeda, Nobuhisa Matsuta, Tetsuya Takeda, Naoshi Hirata, Taku Kawanaka

    Tectonophysics   388 ( 1-4 SPEC. ISS. )   47 - 58   2004.9

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    The northern Fossa Magna (NFM) basin is a Miocene rift system produced in the final stages of the opening of the Sea of Japan. It divides the major structure of Japan into two regions, with north-trending geological structures to the NE of the basin and EW trending structures to the west of the basin. The Itoigawa-Shizuoka Tectonic Line (ISTL) bounds the western part of the northern Fossa Magna and forms an active fault system that displays one of the largest slip rates (4-9 mm/year) in the Japanese islands. Deep seismic reflection and refraction/wide-angle reflection profiling were undertaken in 2002 across the northern part of ISTL in order to delineate structures in the crust, and the deep geometry of the active fault systems. The seismic images are interpreted based on the pattern of reflectors, the surface geology and velocities derived from refraction analysis. The 68-km-long seismic section suggests that the Miocene NFM basin was formed by an east dipping normal fault with a shallow flat segment to 6 km depth and a deeper ramp penetrating to 15 km depth. This low-angle normal fault originated as a comparatively shallow brittle/ductile detachment in a high thermal regime present in the Miocene. The NFM basin was filled by a thick (>6 km) accumulation of sediments. Shortening since the late Neogene is accommodated along NS to NE-SE trending thrust faults that previously accommodated extension and produce fault-related folds on their hanging wall. Based on our balanced geologic cross-section, the total amount of Miocene extension is ca. 42 km and the total amount of late Neogene to Quaternary shortening is ca. 23 km. © 2004 Elsevier B.V. All rights reserved.

    DOI： 10.1016/j.tecto.2004.07.004

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  • The slip-rate along the northern Itoigawa-Shizuoka tectonic line active fault system, central Japan

    Nobuhisa Matsuta, Yasutaka Ikeda, Hiroshi Sato

    Earth, Planets and Space   56 ( 12 )   1323 - 1330   2004

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    The slip-rates on the northern extent of Itoigawa-Shizuoka tectonic line (ISTL) are estimated based on seismic reflection profiles, drill core data and analysis of tectonic geomorphology. The ISTL is a major tectonic line that passes through the Honshu Island of Japan, and its northern and central segments form an active fault system characterized by high slip-rates. In the Kamishiro basin, near the northern end of the ISTL active fault system, the rate of net slip is estimated to be 4.4-5.4 m/kyr over the last 28 ka, with a vertical-separation-rate of 2.2-2.7 m/kyr. In the Omachi area, south of the Kamishiro basin, the Quaternary slip-rate is estimated to be at least 2.9 m/kyr based on the balanced cross-section derived from reflection profiles and surface geology. The dip angle of 30° determined from the Omachi seismic profile suggests a vertical-separation-rate of at least 1.5 m/kyr. Based on compiled evidence from the available geomorphological and paleo-seismological data, vertical-slip-rates of 1.0-2.9 m/kyr are inferred for the region between Hakuba and Toyoshina over the past 3 ka. The northern ISTL exhibits dip-slip-rate of at least 2.9 m/kyr, with a constant average slip-rate of 2.0-5.8 m/kyr since the Early Quaternary. A paleoseismological data and long-term slip-rate along the northern ISTL has potential for a large earthquake. Copyright © The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences.

    DOI： 10.1186/BF03353357

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  • Seismic reflection profiling across the Itoigawa-Shizuoka Tectonic Line at Matsumoto, Central Japan

    Yasutaka Ikeda, Takaya Iwasaki, Hiroshi Sato, Nobuhisa Matsuta, Takeshi Kozawa

    Earth, Planets and Space   56 ( 12 )   1315 - 1321   2004

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    The Itoigawa-Shizuoka Tectonic Line (ISTL) in Central Japan is a fault zone with a very high slip rate during Pliocene-Quaternary time. Our seismic reflection and gravity surveys across the northern segment of the ISTL at Matsumoto have revealed its geometry to a depth of ∼5 km. The fault plane was found to be of fairly low angle, in spite of the surface geologic observations that late Quaternary movements on this fault zone are dominantly strike slip. Partitioning of slip is taking place between the East Boundary Fault (thrust) and the Gofukuji Fault (left-slip), which constitute the fault zone and are parallel to and a few km apart from each other. However, these two faults are found to merge down-dip at a depth as shallow as 1.5 km below the surface. The geometry of the ISTL is significantly discordant with the orientation of the maximum shear stress acting regionally on Central Japan, indicating that the fault plane is of very low strength. Copyright © The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences.

    DOI： 10.1186/BF03353356

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  • Seismological and geological characterization of the crust in the southern part of northern Fossa Magna, central Japan

    Hiroshi Sato, Takaya Iwasaki, Yasutaka Ikeda, Tetsuya Takeda, Nobuhisa Matsuta, Tomoko Imai, Eiji Kurashimo, Naoshi Hirata, Sin'ichi Sakai, Driss Elouai, Taku Kawanaka, Shinji Kawasaki, Susumu Abe, Takeshi Kozawa, Takeshi Ikawa, Yoshimasa Arai, Naoko Kato

    Earth, Planets and Space   56 ( 12 )   1253 - 1259   2004

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    Publishing type：Research paper (scientific journal)  

    The northern Fossa Magna (NMF) is a Miocene rift basin formed in the final stages of the opening of the Sea of Japan. The northern part of Itoigawa-Shizuoka Tectonic Line (ISTL) bounds the western part of the NMF and forms an active fault system that displays one of the largest slip rates in the Japanese islands. Reflection and refraction/wide-angle reflection profiling and earthquake observations by a dense array were undertaken across the northern part of ISTL in order to delineate structures in the crust, and deep geometry of the active fault systems. The ISTL active fault system at depth (ca. 2 km) shows east-dipping low-angle in Omachi and Matsumoto and is extended beneath the Central Uplift Zone and Komoro basin keeping the same dip-angle down to ca. 15 km. The upper part of the crust beneath the Central Uplift Zone is marked by the high Vp and high resistivity zone. Beneath the folded zone of the NMF, the middle to lower crust shows low Vp, low resistivity and more reflective features. The balanced geologic cross-section based on the reflection profiles suggests that the shortening deformation since the late Neogene was produced by the basin inversion of the Miocene low-angle normal fault. Copyright © The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences.

    DOI： 10.1186/BF03353348

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  • Identification of an active fault in the Japanese Alps from DEM-based hill shading

    Takashi Oguchi, Tatsuto Aoki, Nobuhisa Matsuta

    Computers and Geosciences   29 ( 7 )   885 - 891   2003.8

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    Publishing type：Research paper (scientific journal)  

    Shaded-relief images created from digital elevation models (DEMs) are helpful in identifying faults in rugged mountains. Unlike airphoto interpretation, the method enhances lineaments by simulating topographic illumination under varied light directions. Interpretation of shaded-relief images of the Japanese Alps led to the discovery of a lineament unrelated to bedrock structure. Field surveys and analysis of large-scale maps and airphotos reveal the lineament to be a fault with high rates of vertical and lateral slip. The new fault is the southernmost segment of a known adjacent fault, and the rate and direction of its slip provide fresh insight into the late Quaternary history of the fault system. Because previous research mistook the fault scarp for a fluvial terrace scarp, discovery of the fault also changed the correlation of river terraces in the Northern Japanese Alps. The new corrections affect Pleistocene glacial chronology in the upstream area. © 2003 Elsevier Science Ltd. All rights reserved.

    DOI： 10.1016/S0098-3004(03)00083-9

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Books

  • 教育科学を考える

    小川, 容子, 松多, 信尚, 清田, 哲男

    岡山大学出版会  2023.3  （ ISBN:9784904228777 ）

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    Total pages：369p   Language：Japanese

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  • 子どもが問いを生み出す時間 : 総合的な学習の時間の指導を考える

    桑原, 敏典, 清田, 哲男（ Role： Joint author）

    日本文教出版  2022.4  （ ISBN:9784536601306 ）

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    Total pages：191 p   Language：Japanese

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  • Region and life : geographical essays in celebration of the 70th anniversary of the establishment of Okayama university

    Taiga Kadono, Masanori Takayama, Nobuhisa Matta（ Role： Contributor ,  Characteristics of the damages from the Kitatango earthquake along the Gomura fault）

    2022.4 

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  • 地域と生活

    岡山大学

    岡山大学出版会  2022.4  （ ISBN:9784904228746 ）

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    Total pages：319p   Language：Japanese

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  • 教師のための防災学習帳

    小田, 隆史

    朝倉書店  2021.3  （ ISBN:9784254500332 ）

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    Total pages：viii, 100p, 図版 [2] p   Language：Japanese

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  • 東濃地方の地震とその災害

    木股 文昭, 松多信尚

    東濃地震科学研究所  2016 

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  • レジリエンスと地域創生 : 伝統知とビッグデータから探る国土デザイン

    林, 良嗣, 鈴木, 康弘

    明石書店  2015.3  （ ISBN:9784750341507 ）

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    Total pages：249p, 図版viiip   Language：Japanese

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  • 防災・減災につなげるハザードマップの活かし方

    鈴木, 康弘

    岩波書店  2015.3  （ ISBN:9784000058384 ）

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    Total pages：ix, 234p, 図版 [2] p   Language：Japanese

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  • EARTHQUAKE RESEARCH AND ANALYSIS - SEISMOLOGY SEISMOLOGY, SEISMO-TECTONIC AND EARTHQUAKE GEOLOGY

    （ Role： Contributor）

    INTECH  2012 

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  • 第四紀逆断層アトラス

    池田, 安隆, 今泉, 俊文, 東郷, 正美, 平川, 一臣, 宮内, 崇裕, 佐藤, 比呂志

    東京大学出版会  2002.3  （ ISBN:413066705X ）

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    Total pages：iv, 254p   Language：Japanese

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MISC

  • 恵那山断層,猿投山北断層,猿投-境川断層の反射法地震探査—Seismic reflection survey of the Enasan Fault, the Sanageyama North Fault, and the Sanage-Saikagawa Fault

    渡辺 俊樹, 田所 敬一, 石山 達也, 松多 信尚, 鈴木 康弘, 山岡 耕春, 市原 寛, 齋藤 秀雄, 中田 守, 阿部 進

    公益社団法人物理探査学会学術講演会講演論文集 = Proceedings of the SEGJ Conference   148   29 - 32   2023

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    Language：Japanese   Publisher：東京 : 物理探査学会  

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  • Differences changes and problems in disaster prevention education of Japan, Taiwan, and Mainland China Elementary and Junior High Schools

    MATTA Nobuhisa, CHEN Kan

    Proceedings of the General Meeting of the Association of Japanese Geographers   2022s   189   2022

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    Language：Japanese   Publisher：The Association of Japanese Geographers  

    DOI： 10.14866/ajg.2022s.0_189

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  • Topographical characteristics of settlement location in damage area of the anticipated Nankai Trough Earthquake: A comparison with the area damaged by the off the Pacific Coast of Tohoku Earthquake

    Kagohara Kyoko, Kirimura Takashi, Kobayashi Mayu, Matta Nobuhisa

    Proceedings of the General Meeting of the Association of Japanese Geographers   2022s   162   2022

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    Language：Japanese   Publisher：The Association of Japanese Geographers  

    DOI： 10.14866/ajg.2022s.0_162

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  • Reconstruction of sedimentary environments since the Last Glacial period near the Kamishiro fault, Nagano Pref, central Japan

    Shimomura Hitomi, Matta Nobuhisa, Sato Yoshiki, Hirouchi Daisuke

    Proceedings of the General Meeting of the Association of Japanese Geographers   2022s   191   2022

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    Language：Japanese   Publisher：The Association of Japanese Geographers  

    DOI： 10.14866/ajg.2022s.0_191

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  • Evolution of the Kikugawa Lowland based on sediment core analysis

    Hori Kazuaki, Ishii Yuji, Tamura Toru, Sato Yoshiki, Ianazaki Tomio, Nakanishi Toshimichi, Kitagawa Hiroyuki, Hirouchi Daisuke, Mitoma Kayo, Matta Nobuhisa

    Proceedings of the General Meeting of the Association of Japanese Geographers   2022s   158   2022

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    Authorship：Last author   Language：Japanese   Publisher：The Association of Japanese Geographers  

    The topographic features such as marine terraces and coastal plains and their sediments have been used to study the crustal movement and tsunami history associated with the repeated earthquakes in the Nankai Trough. In order to extract valuable information on crustal movement and tsunamis through the analysis of these landforms and sediments, it is necessary to clarify the relationship between the landforms and strata formation and glacial sea-level change. We report the results of analysis of sediment cores obtained from the Kikugawa lowland in the eastern part of the Enshunada and discuss the formation process of the Kikugawa lowland.

    DOI： 10.14866/ajg.2022s.0_158

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  • The Study of Child-rearing Care Support of the People who Suffered by Floods-Focusing on Allocation of Child-rearing Care Work-

    Sakamoto Mayumi, Hiraoka Atsuko, Koyama Maki, Matta Nobuhisa, Hara Kohei

    Journal of Social Safety Science   39   315 - 323   2021.11

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    Language：Japanese   Publisher：Institute of Social Safety Science  

    This study focuses on child-rearing care support for the people who suffered by floods. In case houses are affected by floods, people have to cleanup, dry and repair houses. People have to evacuate shelters or temporary houses until their own home repair finish. The change of living environment sometime causes difficulty in balancing works, household works and parenting works. The study analyzes child-rearing work balance focusing work allocation among family, government support and community support through case study of Mabi Town, Kurashiki City, Japan which suffered by the 2018 July heavy rain disaster. It tries to identify post-disaster parenting work balance problems and discusses how to balance those works.

    DOI： 10.11314/jisss.39.315

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  • トクシュウ ボウサイ キョウイク オ イカス 「 チリ ソウゴウ 」 エ

    マツタ ノブヒサ, ヤノ ケイジ

    91 ( 5 )   449 - 453   2021.5

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  • The Study on Evacuation Triggers during Heavy Rain -Based on Evacuation Behavior Survey of 2018 Western Japan Heavy Rain Disaster- Reviewed

    SAKAMOTO Mayumi, MATTA Nobuhisa, HIROI U, KOYAMA Maki

    Journal of Japan Society for Natural Disaster Science   39 ( 4 )   439 - 457   2021

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    Language：Japanese   Publisher：Japan Society for Natural Disaster Science  

    Recent heavy rain disasters in Japan showed the fact that although government issuedevacuation information, there were people who did not evacuate. This indicates that evacuationinformation based on science, which is institutionalized as a decision-making mechanismfor government, is not properly utilized by public. This study conducted surveys to residentsof Mabi Town, Kurashiki City, Japan, which was severely flooded due to the Western Japanheavy rain of July, 2018. The study tried to identify factors which triggered risk awarenessof residents comprehensively, and examined how those factors contributed to evacuationdecision-makings using "Evacuation Act Curve," the method adapted to the "Recovery Curve"surveys. As a result, the study revealed the fact that residents were tend to evacuate based onchanges in familiar environment rather than science-based information, which means thatdisaster information was still not considered as familiar information.

    DOI： 10.24762/jndsj.39.4_439

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  • Geographical Efforts to hand down the experience of flood damage in the Okada area of Mabi-cho, Kurashiki City

    松多信尚

    日本地理学会発表要旨集   2021 ( 99 )   148 - 148   2021

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    Language：Japanese   Publisher：The Association of Japanese Geographers  

    <p>In the Okada district of Mabi-cho, Kurashiki City, which experienced the heavy rain disaster in western Japan in 2018, residents are trying to hand down the flood disaster experience so that they will never have a tragic experience again. In that activity, disaster prevention and mitigation measures were divided into three categories: evacuation, living, and succession. For the result, Effective disaster prevention and mitigation means "expanding the scope of assumptions by understanding natural phenomena and modern society, and acquiring the ability to respond to unexpected encounters, rather than thoroughly implementing evacuation manuals within expectations."</p>

    DOI： 10.14866/ajg.2021s.0_148

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  • 1:25,000活断層図 糸魚川-静岡構造線断層帯及び境峠・神谷断層帯とその周辺「諏訪改訂版」解説書

    松多信尚

    1:25,000活断層図 糸魚川-静岡構造線断層帯及び境峠・神谷断層帯とその周辺「諏訪 改訂版」解説書 令和3年(CD-ROM)   2021

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  • S波ランドストリーマー反射法探査およびS波速度検層による海岸平野下の浅部地下構造イメージング—Imaging of near surface structure beneath a coastal plain utilizing Landstreamer S-wave reflection survey and downhole S-wave measurements

    稲崎 富士, 松多 信尚, 楮原 京子, 岡田 真介, 中西 利典, 堀 和明, 中埜 貴元

    公益社団法人物理探査学会学術講演会講演論文集 = Proceedings of the SEGJ Conference   145   181 - 184   2021

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    Language：Japanese   Publisher：物理探査学会  

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  • 南海トラフ地震を想定した救援物資輸送ルートの検討

    佐々木 達, 荒木 一視, 楮原 京子, 熊谷 美香, 田中 耕市, 中村 努, 松多 信尚

    E-journal GEO   15 ( 1 )   101 - 114   2020

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    Language：Japanese   Publisher：公益社団法人 日本地理学会  

    DOI： 10.4157/ejgeo.15.101

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    Other Link： https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-18H00772/

  • Characteristics of Flood Trace Heights in Mabicho, Kurashiki City by the 2018 Torrential Rain Reviewed

    丸山雄大, 松多信尚, 後藤秀昭, 中田高, 田中圭

    地理科学   75 ( 3 )   117 - 126   2020

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    Language：Japanese   Publisher：THE JAPANESE SOCIETY FOR GEOGRAPHICAL SCIENCES  

    DOI： 10.20630/chirikagaku.75.3_117

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  • Trigger of Start Evacuating at the Time of Disaster-Case of the Evacuation Behavior on 2018 Western Japan Heavy Rain Disaster in mabi-cho Kurashiki city-

    松多信尚, 久本侑奈, 久本侑奈

    日本地理学会発表要旨集   2020 ( 98 )   143 - 143   2020

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    Language：Japanese   Publisher：The Association of Japanese Geographers  

    <p>Flood is a disaster that can be evacuated. For the reason, information such as hazard maps are released and evacuation advisories are provided, but the residents are not able to take sufficient evacuation actions at a disaster. Therefore, in order to clarify the trigger of the actual evacuation behavior, we conducted an investigation using the evacuation act curve for the victims of the Mabi flood disaster. As a result, it was found that there are three types of evacuation behavior: (1) the type that evacuation awareness increases sharply when triggered, (2) the type that evacuation awareness gradually increases, (3) the type that does not change.We have to consider policies by type. We have to consider measures for each type. We propose to provide appropriate information through leagional geography class at the school.</p>

    DOI： 10.14866/ajg.2020a.0_143

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  • Tectonic landform and rock-controlled landform along fault trace of the Aceh segment, the northernmost Sumatran Fault

    副田宜男, 堤浩之, 松多信尚, ISMAIL Nazli, ALI Bukhari

    日本地球惑星科学連合大会予稿集(Web)   2020   2020

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  • GPR survey for estimating the internal structure of the beach levee formed in the coastal lowland of Enshunada Sea

    中埜貴元, 松多信尚, 堀和明, 廣内大助, 杉戸信彦, 佐藤善輝, 石山達也

    日本地球惑星科学連合大会予稿集(Web)   2020   2020

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  • 倉敷市真備町の土地利用変遷-特に住宅地の変遷に着目して-

    松多信尚, 洪水麻里, 西山弘祥, 石黒聡士

    地域地理研究(Web)   25 ( 2 )   2020

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  • 災害時における住民の避難に至る意識の変動-平成30年西日本豪雨倉敷市真備町を例に-

    松多信尚, 久本侑奈

    地域地理研究(Web)   25 ( 2 )   2020

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  • 平成30年7月豪雨から2年後の被災地住民の防災意識-倉敷市真備町岡田・辻田地区住民意識調査より-

    阪本真由美, 小山真紀, 松多信尚, 平岡敦子

    日本災害情報学会学会大会予稿集   22nd (Web)   2020

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  • Paleoseismology of the northren part of Kamishiro fault, ISTL active fault zone, central Japan

    廣内大助, 松多信尚, 石山達也, 安江健一, 杉戸信彦, 竹下欣宏, 藤田奈津子, 澤祥, 水谷光太郎, 谷口薫

    日本地球惑星科学連合大会予稿集(Web)   2020   2020

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  • High-resolution shear-wave seismic reflection surveys across the Kamishiro fault, Itoigawa-Shizuoka Tectonic Line active fault system, central Japan

    池口直毅, 松多信尚, 楮原京子, 岡田真介, 廣内大助, 石山達也, 野田克也, 佐藤比呂志

    物理探査学会学術講演会講演論文集   140   55 - 58   2019

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  • 小田川の地形条件と堤外地の2018年の土砂堆積

    黒木貴一, 品川俊介, 松多信尚

    日本応用地質学会研究発表会講演論文集   2019   2019

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  • 2018年西日本豪雨 岡山洪水災害の地形・地質的背景

    鈴木茂之, 中曽根茂樹, 足立勝治, 向山栄, 小俣雅志, 小林浩, 品川俊介, 平野昌繁, 松多信尚, 黒木貴一

    平成30年7月豪雨災害(西日本豪雨災害)調査団報告書-広域・激甚化する災害に学び、次の災害に備える   2019

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  • Tectonic geomorphology and imbricate thrust structures of Agoyama Fault imaged by seismic reflection profiling, Fujikawa-kako Fault Zone, central Japan

    Ishiyama Tatsuya, Kato Naoko, Sato Hiroshi, Hirouchi Daisuke, Matsuta Nobuhisa

    Annual Meeting of the Geological Society of Japan   2019   237 - 237   2019

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    Language：Japanese   Publisher：The Geological Society of Japan  

    DOI： 10.14863/geosocabst.2019.0_237

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  • Heavy rain disaster in July 2018 and characteristics on geomorphic quantity of Oda river

    Kuroki Takahito, Shinagawa Shunsuke, Matta Nobuhisa

    Proceedings of the General Meeting of the Association of Japanese Geographers   2019 ( 96 )   25 - 25   2019

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    Language：Japanese   Publisher：The Association of Japanese Geographers  

    <p>We investigated the heavy rain disaster in July 2018 and the characteristics on geomorphic quantity of Oda river.</p>

    DOI： 10.14866/ajg.2019a.0_25

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  • Relationship between development of beach ridges and seismic crustal movements in Kikugawa Lowland in the Shizuoka Prefecture, Central Japan

    Hayata Keisuke, Matsuta Nobuhisa, Hirouchi Daisuke

    Proceedings of the General Meeting of the Association of Japanese Geographers   2019 ( 95 )   306 - 306   2019

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    Language：Japanese   Publisher：The Association of Japanese Geographers  

    DOI： 10.14866/ajg.2019s.0_306

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  • 高分解能浅層反射法地震探査から見た神城断層先端部の構造と2014年長野県北部の地震の地表地震断層の関係

    池口直毅, 松多信尚, 楮原京子, 岡田真介, 廣内大助, 戸田茂, 石山達也, 小池太郎, 野田克也, 佐藤比呂志

    日本地震学会秋季大会講演予稿集(CD-ROM)   2019   2019

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  • 濃尾地震の被害から検証する岐阜-一宮線

    松多信尚, 松多信尚, 木股文昭

    日本地球惑星科学連合大会予稿集(Web)   2019   2019

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  • 地理的特性に焦点をあてた防災教育への提言(「100年続く防災を考える」)

    川上賢太, 松多信尚

    日本地球惑星科学連合大会予稿集(Web)   2019   2019

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  • 糸魚川-静岡構造線活断層系神城断層における高解像度極浅層S波反射法地震探査

    池口直毅, 松多信尚, 楮原京子, 岡田真介, 廣内大助, 石山達也, 野田克也, 佐藤比呂志

    日本地球惑星科学連合大会予稿集(Web)   2019   2019

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  • 糸魚川-静岡構造線断層帯神城断層南部における活動履歴調査

    水谷光太郎, 廣内大助, 松多信尚, 石山達也, 杉戸信彦, 安江健一, 竹下欣宏, 藤田奈津子, 澤祥, 道家涼介, 丸山陽央, 池田一貴

    日本地球惑星科学連合大会予稿集(Web)   2019   2019

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  • 平成30年7月豪雨における倉敷市真備町の水害の時間経緯とその特徴

    松多信尚, 丸山雄大, 森脇敏

    地域地理研究(Web)   24 ( 2 )   2019

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  • 平成30年7月豪雨における倉敷市真備町における避難行動

    松多信尚, 江田志都香, 西川紗永

    地域地理研究(Web)   24 ( 2 )   2019

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  • 災害遺構の保存について -倉敷市真備町を例に-

    松多信尚, 山口雄治, 森脇敏, 川上賢太

    地域地理研究(Web)   24 ( 2 )   2019

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  • 歴史地震にみる震災後の地場産業の復興(1)1891年濃尾地震における東濃の陶器産業と尾張の織物産業

    木股文昭, 松多信尚

    歴史地震(Web)   ( 34 )   2019

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  • Persistent and time-dependent crustal deformation in northern Fossa Magna and its tectonic implications

    SAGIYA Takeshi, KUMAGAI Koki, MENESES-GUTIERREZ Angela, MATSUTA Nobuhisa, HIROUCHI Daisuke, MATSUHIRO Kenjiro, OKUDA Takashi

    日本地球惑星科学連合大会予稿集(Web)   2019   2019

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  • The study of applicability of the geophysical exploration methods for the strike-slip fault (part 1; shallow P-wave seismic reflection and refraction survey, CSAMT survey, and gravity survey) : the case study of the Go-mura fault zone and Yamada fault zone

    Okada Shinsuke, Yamaguchi Satoru, Matsubara Yoshikazu, Yamamoto Masato, Todokoro Hitoshi, Imai Mikihiro, Jomori Akira, Sakashita Susumu, Imaizumi Toshifumi, Okada Atsumasa, Nakamura Norihiro, Fukuchi Tatsuro, Matta Nobuhisa, Kagohara Kyoko, Toda Shigeru

    BUTSURI-TANSA(Geophysical Exploration)   71   103 - 125   2018

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    Language：Japanese   Publisher：The Society of Exploration Geophysicists of Japan  

    <p>The geometry/angle of the deeper extension of active fault is one of the fundamental information to evaluate the magnitude of inland earthquake associated with active faulting. The information is mainly revealed by geophysical exploration that is executed across the active fault. Although the geophysical explorations were scarcely applied for strike-slip fault in Japan, we discuss the applicability of several geophysical explorations, seismic reflection and refraction survey, CSAMT (controlled source audio-magnetotelluric) survey and gravity survey for strike-slip fault in this study. The study area is located in northwest area in Kinki region in Japan, and Go-mura fault zone and Yamada fault zone are distributed in a granite area (Miyazu granite). In the seismic reflection profile, discontinuity and inflection of reflector shows the deeper geometry of active fault in 200-300 m below the surface of the ground. In some profile, discordance between subsurface structure and slip direction of the active fault were shown. Hence, the comparison between seismic reflection profile and other geophysical explorations is important in the interpretation of subsurface geometry of the active fault. Although, the seismic refraction image cannot define the strict angle of the active fault in principle, the image well indicates the low-velocity layer crushed by the strike-slip faulting. In the CSAMT survey, low-specific resistance area extended in depth clearly shows the geometry and angle of deeper part of active fault. In some image, pseudo-specific resistance can be seen in some CSAMT image, comparison to other information of geophysical survey is necessary for interpretation. Because the vertical displacement is not dominant in strike-slip faulting, the gravity survey across the strike-slip fault is generally insufficient method to detect the fault. Dense spacing of gravity stations and precise measurement allow sensing the Bouguer gravity anomaly associated with strike-slip faulting.</p>

    DOI： 10.3124/segj.71.103

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  • Triangulation scale error caused by the 1894 Shonai earthquake: a possible cause of erroneous interpretation of seismic potential along the Japan Trench

    Sagiya Takeshi, Matta Nobuhisa, Ohta Yusaku

    Earth, Planets and Space (Web)   70 ( 1 )   2018

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  • The study of applicability of the geophysical exploration methods for the strike-slip fault (part 1; shallow P-wave seismic reflection and refraction survey, CSAMT survey, and gravity survey) : the case study of the Go-mura fault zone and Yamada fault zone

    岡田真介, 坂下晋, 今泉俊文, 岡田篤正, 中村教博, 福地龍郎, 松多信尚, 楮原京子, 戸田茂, 山口覚, 松原由和, 山本正人, 外處仁, 今井幹浩, 城森明

    物理探査(Web)   71   2018

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  • Triangulation scale error caused by the 1894 Shonai earthquake: a possible cause of erroneous interpretation of seismic potential along the Japan Trench

    SAGIYA Takeshi, MATTA Nobuhisa, OHTA Yusaku

    Earth, Planets and Space (Web)   70 ( July )   2018

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    Horizontal crustal strain in the Tohoku area during the twentieth century based on triangulation showed N-S extension and E-W contraction was not significant. This feature was one of the reasons why the 2011 Tohoku-oki earthquake was unexpected for many scientists. The first triangulation conducted in the late nineteenth century used a length scale defined by baseline surveys, direct measurements of short (2-10 km) baselines with steel rods. The Shionohara baseline in the Yamagata prefecture was measured in May-July 1894 and the 1894 Shonai (M7.0) earthquake occurred in its western neighbor 3 months after the measurement. The earthquake possibly elongated the baseline by as large as 5 cm or 10 ppm. However, the original length measured before the earthquake was used for the network adjustment of the entire triangulation network, causing extensive underestimation of the length scale of the network as large as 5-10 ppm in northeast Japan. The scale error effect was comparable to tectonic deformation signal over 100 years. The baseline length was re-surveyed in 2012, 1 year after the Tohoku-oki earthquake, and the result is consistent with the hypothesis of scale bias considering interseismic deformation.

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  • The distribution of net slip on the 2014 Kamishiro fault earthquake in central Japan

    Matta Nobuhisa matsuta, Ikeguchi Naoki, OKADA Shinsuke, KAGOHARA Kyoko, ISHIYAMA Tatsuya, HIROUCHI Daisuke, crew Kamishiro fault seismic survey

    Proceedings of the General Meeting of the Association of Japanese Geographers   2018 ( 94 )   117 - 117   2018

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    DOI： 10.14866/ajg.2018a.0_117

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  • Faulting event of the Northern middle part of Kamishiro fault, ISTL active fault zone, central Japan

    Hirouchi Daisuke, Matsuta Nobuhisa

    Proceedings of the General Meeting of the Association of Japanese Geographers   2018 ( 93 )   305 - 305   2018

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    DOI： 10.14866/ajg.2018s.0_000305

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  • Perspectives in active fault studies: Celebrated symposium for the 10th anniversary of the society Reviewed

    Goto Hideaki, Matta Nobuhisa, Kumahara Yasuhiro

    Active Fault Research   2018 ( 49 )   51 - 55   2018

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    DOI： 10.11462/afr.2018.49_51

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  • 地表地震断層近傍にみられる地震災害の特殊性-三河地震,北丹後地震,濃尾地震を例に-

    松多信尚, 松多信尚, 木股文昭

    日本地震工学シンポジウム論文集(CD-ROM)   15th   2018

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  • 平成30年7月豪雨災害における避難行動に関する考察-岡山県倉敷市真備町の住民意識調査より-

    阪本真由美, 松多信尚, 廣井悠

    日本災害情報学会学会大会予稿集   20th   2018

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  • 糸魚川-静岡構造線断層帯北部における地殻変動の時間変化と活断層間の力学的相互作用

    熊谷光起, 鷺谷威, 鷺谷威, MENESES-GUTIERREZ Angela, ZHANG Xuelei, 松多信尚, 廣内大助, 松廣健二郎, 奥田隆

    日本測地学会講演会要旨   130th   2018

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  • Persistent and time-dependent characteristics of crustal deformation in the Central-Northern Nagano area associated with the 2011 Tohoku-oki and the 2014 Northern Nagano earthquakes

    KUMAGAI Koki, SAGIYA Takeshi, MENESES-GUTIERREZ Angela, ZHANG XUELEI, MATSUTA Nobuhisa, HIROUCHI Daisuke, MATSUHIRO Kenjiro, OKUDA Takashi

    日本地球惑星科学連合大会予稿集(Web)   2018   2018

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  • 糸魚川-静岡構造線活断層系神城断層における極浅層S波反射法地震探査

    池口直毅, 松多信尚, 楮原京子, 岡田真介, 廣内大助, 石山達也, 野田克也, 高山正教, 川上賢太, 原田稚子, 福井恒平, 丸山雄大, 藤井遥, 上田航, 西川智樹, 渡辺隆輝, 佐藤比呂志

    日本地球惑星科学連合大会予稿集(Web)   2018   2018

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  • Seismic and inter-seismic ground surface deformations of the Murono mud volcano (central Japan): a laser scanning approach

    HAYAKAWA Yuichi S., KUSUMOTO Shigekazu, MATTA Nobuhisa

    Progress in Earth and Planetary Science (Web)   4 ( Feb )   3   2017

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    A small mud volcano in Murono, Niigata Prefecture, north-central Japan, shows active ground surface displacements, not only when large earthquakes occur in the region but also during quiescent periods between earthquake events. The site recently underwent abrupt deformations due to strong regional earthquakes in 2004, 2007, 2011, and 2014, while gradual surface deformations were reported during quiescent periods between the earthquakes. To detect the spatial distribution of the changes in the mud volcano's ground surface elevation, we carried out multi-temporal terrestrial laser scanning. Point cloud datasets were registered at different times by minimizing the distance between the closest points in different clouds for stable ground features, which revealed centimeter-to decimeter-scale deformations around the domain of the conspicuous uplift. The spatial distribution of the deformation triggered by the earthquakes, including both central uplift and peripheral subsidence, exhibits an elliptical pattern, on which open crack fractures, associated with the earthquake-triggered uplift, were formed. The displacement and stress fields for the earthquakes were modeled numerically, and anomalously high pressure and/or weakening of the surficial materials was expected for the formation of fractures in the local domain. In contrast, continuous uplift was observed during the inter-seismic quiescent periods, the domain of which seems to have changed after the strong earthquake in 2014. In the coming years, further measurements will be necessary to unravel the physical subsurface mechanics of the mud volcano.

    DOI： 10.1186/s40645-016-0116-3

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  • Active fault in the Kibi Plateau, Southwest Japan

    Matta Nobuhisa

    Annual Meeting of the Geological Society of Japan   2017   38 - 38   2017

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    DOI： 10.14863/geosocabst.2017.0_038

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  • Earthquake-induced surface deformations in a small mud volcano: multi-temporal high-definition measurements using TLS and UAS-SfM

    HAYAKAWA Yuichi S., KUSUMOTO Shigekazu, MATSUTA Nobuhisa

    日本地球惑星科学連合大会予稿集(Web)   2017   2017

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  • 稠密GNSS観測から推定される阿寺断層の応力蓄積過程

    熊谷光起, 鷺谷威, 松多信尚

    日本測地学会講演会要旨   128th   2017

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  • 津軽山地東縁における反射法地震探査

    楮原京子, 越後智雄, 岡田真介, 戸田茂, 井上直人, 宮内崇裕, 今泉俊文, 小坂英輝, 三輪敦志, 坂下晋, 松原由和, 阿部恒平, 黒澤英樹, 松多信尚, 石山達也

    日本地球惑星科学連合大会予稿集(Web)   2017   2017

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  • 北丹後地震における全壊家屋-犠牲者比率からみる地表地震断層近傍の人的被害について

    角野大河, 松多信尚

    日本地球惑星科学連合大会予稿集(Web)   2017   2017

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  • ジオパークにおける教育的実践例とその特徴

    寺本結哉, 松多信尚

    日本地球惑星科学連合大会予稿集(Web)   2017   2017

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  • Tectonic Loading of the Atera Fault inferred from Dense GNSS Observation

    KUMAGAI Koki, SAGIYA Takeshi, MATSUTA Nobuhisa

    日本地球惑星科学連合大会予稿集(Web)   2017   2017

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  • 熊本県益城町を対象とした2016年熊本地震に伴う地区別死者数の分析

    中嶋唯貴, 岡田成幸, 篠田茜, 松多信尚

    日本地震学会秋季大会講演予稿集(CD-ROM)   2017   2017

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  • 多チャンネル電磁探査装置を用いた高密度CSAMT探査の活構造調査への適用

    坂下晋, 小田佑介, 山下善弘, 小林貴幸, GROOM Douglas, BIN He, WANG Fei, 越後智雄, 楮原京子, 岡田真介, 戸田茂, 井上直人, 宮内崇裕, 今泉俊文, 小坂英輝, 三輪敦志, 松原由和, 阿部恒平, 黒澤英樹, 松多信尚, 石山達也

    日本地球惑星科学連合大会予稿集(Web)   2017   2017

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  • High-resolution Digital Surface Models of Surface Rupture Associated with the 2016 Kumamoto Earthquake, by Using Unmanned Aerial Vehicle Photography

    36 ( 3 )   214 - 217   2016.7

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  • 話題提供 日本の中でみた瀬戸内地方の土砂災害の特徴 (2015年度 地域地理科学会 大会記録) -- (シンポジウム 「瀬戸内」の災害を考える : 広域災害にむけて)

    松多 信尚

    地域地理研究 = Journal of systematic regional geography   22 ( 1 )   67 - 69   2016.6

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  • Application of terrestrial laser scanning for detection of ground surface deformation in small mud volcano (Murono, Japan)

    HAYAKAWA Yuichi, KUSUMOTO Shigekazu, MATTA Nobuhisa

    Earth, Planets and Space (Web)   68 ( July )   114   2016

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    We perform terrestrial laser scanning (TLS) to detect changes in surface morphology of a mud volcano in Murono, north-central Japan. The study site underwent significant deformation by a strong earthquake in 2011, and the surface deformation has continued in the following years. The point cloud datasets were obtained by TLS at three different times in 2011, 2013 and 2014. Those point clouds were aligned by cloud-based registration, which minimizes the closest point distance of point clouds of unchanged ground features, and the TLS-based point cloud data appear to be suitable for detecting centimeter-order deformations in the central domain of the mud volcano, as well as for measurements of topographic features including cracks of paved ground surface. The spatial patterns and accumulative amount of the vertical deformation during 2011-2014 captured by TLS correspond well with those previously reported based on point-based leveling surveys, supporting the validity of TLS survey.

    DOI： 10.1186/s40623-016-0495-0

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  • Application of terrestrial laser scanning for detection of ground surface deformation in small mud volcano (Murono, Japan) 6. Geodesy

    Hayakawa, Yuichi S., Kusumoto, Shigekazu, Matta, Nobuhisa

    Earth, Planets and Space   68 ( 1 )   2016

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  • Tectonic geomorphological study of the surface rupture associated with the 2014 Kamishiro fault earthquake at Warabidaira, Hakuba Village, central Japan

    MATSUTA Nobuhisa, SUGITO Nobuhiko, HIROUCHI Daisuke, IKEDA Kazutaka, SAWA Hiroshi, WATANABE Mitsuhisa, SUZUKI Yasuhiro

    Proceedings of the General Meeting of the Association of Japanese Geographers   2016 ( 89 )   100244 - 100244   2016

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    DOI： 10.14866/ajg.2016s.0_100244

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  • Delivering Relief Supplies: Geography's Contribution to Reducing the Secondary Damage from Widespread Disasters

    Hitoshi ARAKI, Nobuyuki IWAMA, Kyoko KAGOHARA, Mika KUMAGAI, Koichi TANAKA, Tsutomu NAKAMURA, Nobuhisa MATTA

    E-journal GEO   11 ( 2 )   526 - 551   2016

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    <p>Following the Great East Japan Earthquake, the contribution of geography was discussed from the viewpoint of delivering relief supplies after widespread disasters. Possible emergencies, obstacles, and counterplans were analyzed with the Nankai megathrust earthquake in mind. The Pacific coast of southeastern Japan, especially the Kii Peninsula, southern Shikoku, and eastern Kyushu, was an area significantly affected by the earthquake. The area was characterized by an aging population, little public transport, and poor transportation infrastructure. In addition, with the declining self-sufficiency of rural life, many commodities, including foodstuffs, consumed by rural residents are supplied from urban areas. In this current situation in Japan, delays and bottlenecks in the delivery of supplies to disaster-hit areas could cause major disruptions in relief activities. Therefore, rapid, effective relief transport systems and emergency stock systems are needed to reduce the damage. However, comprehensive approaches to these aspects lag behind in comparison with disaster-prevention measures and disaster-recovery assistance.</p>

    DOI： 10.4157/ejgeo.11.526

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    Other Link： https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15K01169/

  • Evaluation of High-resolution Digital Surface Models of Surface Rupture Associated with the 2014 Kamishiro Fault Earthquake, Central Japan, Using Unmanned Aerial Vehicle Photography and SfM-MVS Analysis

    ISHIGURO Satoshi, SUZUKI Yasuhiro, KUMAHARA Yasuhiro, GOTO Hideaki, NAKATA Takashi, MATSUTA Nobuhisa, SUGITO Nobuhiko, HIROUCHI Daisuke, WATANABE Mitsuhisa, SAWA Hiroshi

    Journal of The Remote Sensing Society of Japan   36 ( 2 )   107 - 116   2016

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    Surface ruptures associated with the 2014 Kamishiro fault earthquake (Mj 6.7), appeared along the Itoigawa-Shizuoka Tectonic line active fault system in the northern part of Nagano Prefecture, central Japan. We photographed it with digital cameras mounted on an unmanned aerial vehicle (UAV). Digital surface models (DSMs) were generated from the acquired photographs by applying SfM-MVS technology. The UAVs used in this study were the F450 and Phantom 2 manufactured by DJI Inc., and the cameras were the GR model manufactured by RICOH Inc. and were attached to each UAV for aerial photography. The ground control points required for generating DSMs using SfM-MVS analysis were measured using an RTK-GNSS (Leica GPS900), and the topographic profiles used for the accuracy assessment of the DSMs were measured in situ using a total station (Leica TCR705) and digital auto level (SOKKIA SDL50).<BR>As a result, we were able to create DSMs and ortho-photographs at the resolution of a few centimeters. The accuracy was assessed by comparing the topographic profiles measured by the total station and leveling with those generated by the DSMs. Validation against the nine topographic profiles revealed that the DSM had a relative height error of 4.0cm with an average standard deviation.<BR>Taking photographs from a UAV is one of the quickest and most cost-effective methods to record detailed surface topography. Generating a DSM of surface ruptures using UAV photography with SfM-MVS is particularly advantageous because ruptures will change their features quickly, and surface topographic variations of 10 cm or less cannot be recognized in field observations.

    DOI： 10.11440/rssj.36.107

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  • 2016年熊本地震の地表地震断層

    後藤秀昭, 熊原康博, 中田高, 石黒聡, 石村大輔, 石山達也, 岡田真介, 楮原京子, 柏原真太郎, 金田平太郎, 杉戸信彦, 鈴木康弘, 竹竝大士, 田中圭, 田中知季, 堤浩之, 遠田晋次, 廣内大助, 松多信尚, 森木ひかる, 吉田春香, 渡辺満久

    日本地球惑星科学連合大会予稿集(Web)   2016   2016

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  • 1:25,000都市圏活断層図白馬岳・大町

    廣内大助, 澤祥, 石村大輔, 岡田真介, 楮原京子, 後藤秀昭, 杉戸信彦, 鈴木康弘, 松多信尚

    1:25,000都市圏活断層図白馬岳・大町 一部改訂版 平成28年   2016

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  • Surface fault ruptures associated with the 14 April foreshock (Mj 6.5) of the 2016 Kumamoto earthquake sequence, southwest Japan

    SUGITO Nobuhiko, GOTO Hideaki, KUMAHARA Yasuhiro, TSUTSUMI Hiroyuki, NAKATA Takashi, KAGOHARA Kyoko, MATSUTA Nobuhisa, YOSHIDA Haruka

    Earth, Planets and Space (Web)   68 ( Nov )   2016

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  • 熊本地震にともなう二重峠地震帯の活動

    中田高, 後藤秀昭, 田中圭, 池辺伸一郎, 隈元崇, 松多信尚, 楮原京子, 渡辺満久, 鈴木康弘, 高田圭太

    日本地震学会秋季大会講演予稿集   2016   2016

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  • 郷村断層帯・山田断層帯において実施した各種物理探査とその有効性(その1:S波極浅層反射法地震探査,高密度電気探査)

    坂下晋, 岡田真介, 今泉俊文, 戸田茂, 楮原京子, 松多信尚, 山口覚, 山本正人, 今井幹浩, 外處仁

    日本地球惑星科学連合大会予稿集(Web)   2016   2016

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  • 郷村断層帯・山田断層帯において実施した各種物理探査とその適用性(その2:P波反射法地震探査,屈折法地震探査,CSAMT探査,重力探査)

    岡田真介, 今泉俊文, 坂下晋, 楮原京子, 戸田茂, 松多信尚, 山口覚, 山本正人, 今井幹浩, 外處仁, 松原由和

    日本地球惑星科学連合大会予稿集(Web)   2016   2016

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  • 2016年熊本地震の「前震」に伴う益城町島田・小池~嘉島町井寺付近の地表変形

    杉戸信彦, 後藤秀昭, 熊原康博, 中田高, 楮原京子, 堤浩之, 松多信尚, 吉田春香

    日本地球惑星科学連合大会予稿集(Web)   2016   2016

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  • 2014年長野県北部の地震(Mw6.2)の地表地震断層を横切る反射法地震探査

    岡田真介, 松多信尚, 小鹿浩太, 川崎悠介, 松原由和, 遠田晋次

    日本地球惑星科学連合大会予稿集(Web)   2016   2016

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  • 2016年熊本地震による阿蘇カルデラの北部低地に見られる亀裂と地震断層:地上調査と低空撮画像の解析による検討

    田中圭, 中田高, 松多信尚, 楮原京子, 竹竝大士, 隈元崇, 森木ひかる

    日本地球惑星科学連合大会予稿集(Web)   2016   2016

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  • 神城断層(糸魚川静岡構造線活断層)の活動履歴-白馬村蕨平における変動地形学的調査

    松多信尚, 杉戸信彦, 廣内大助, 池田一貴, 澤祥, 渡辺満久, 鈴木康弘

    日本地球惑星科学連合大会予稿集(Web)   2016   2016

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  • Distribution of surface rupture associated the 2016 Kumamoto earthquake and its significance

    KUMAHARA Yasuhiro, GOTO Hideaki, NAKATA Takashi, ISHIGURO Satoshi, ISHIMURA Daisuke, ISHIYAMA Tatsuya, OKADA Shinsuke, KAGOHARA Kyoko, KASHIHARA Shintaro, KANEDA Heitaro, SUGITO Nobuhiko, SUZUKI Yasuhiro, TAKENAMI Daishi, TANAKA Kei, TANAKA Tomoki, TSUTSUMI Hiroyuki, TODA Shinji, HIROUCHI Daisuke, MATSUTA Nobuhisa, MITA Tomokazu, MORIKI Hikaru, YOSHIDA Haruka, WATANABE Mitsuhisa

    日本地球惑星科学連合大会予稿集(Web)   2016   2016

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  • Geographies of relief goods transportation

    ARAKI Hitoshi, IWAMA Nobuyuki, KAGOHARA Kyoko, TANAKA Koichi, NAKAMURA Tsutomu, MATTA Nobuhisa

    Proceedings of the General Meeting of the Association of Japanese Geographers   2015 ( 88 )   100001 - 100001   2015

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    DOI： 10.14866/ajg.2015a.0_100001

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  • Significance of the Tsunami Run-up Height Map for the 2011 off the Pacific coast of Tohoku earthquake

    Sugito Nobuhiko, Matsuta Nobuhisa, Ishiguro Satoshi, Sano Shigeki, Uchida Chikara, Senda Yoshimichi, Sakaue Hiroyuki, Suzuki Yasuhiro

    Proceedings of the General Meeting of the Association of Japanese Geographers   2015 ( 87 )   100166 - 100166   2015

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    DOI： 10.14866/ajg.2015s.0_100166

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  • Slip rate and timing of faulting on the the Kamishiro fault revealed at Shinden and Oide, Hokujo, Hakuba Village, central Japan Reviewed

    Sugito Nobuhiko, Taniguchi Kaoru, Matsuta Nobuhisa, Sawa Hiroshi, Tajikara Masayoshi, Nozawa Tatsujiro, Minaguro Takeshi

    Active Fault Research   2015 ( 43 )   109 - 118   2015

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    Language：Japanese   Publisher：Japanese Society for Active Fault Studies  

    <p>An Mj 6.7 earthquake struck the northern part of the Nagano Prefecture, central Japan, at 22:08 JST on November 22, 2014. The earthquake was named 2014 Naganoken-hokubu earthquake, and its coseismic surface rupture has been identified along the northern part of the Kamishiro fault in the northernmost part of the Itoigawa-Shizuoka Tectonic Line active fault system. We have conducted 1) aerial-photograph interpretation, 2) field explorations, 3) photogrammetric analysis, and 4) drilling and pit excavation surveys on the northern part of the Kamishiro fault since 2005, in order to better estimate slip rates and timing of faulting on the fault. At the Shinden site, the Aira-Tanzawa volcanic ash (ca. 30 ka) was identified in the L1 terrace-surface deposit. In addition, the age of L2 terrace surface was estimated at ca. 5 ka. Because the amounts of vertical offset of the L2 terrace surface are 8.0 m and 6.5-7.0 m at the Shinden and Oide sites, vertical slip rates can be calculated to be 1.6 mm/yr and 1.3-1.4 mm/yr, respectively. We also revealed subsurface stratigraphy in the down-thrown side of the Kamishiro fault at the Oide site, and identified three possible paleoseismic events that occurred ca. 1,000-1,300 years ago, 500-600 years ago, and after 300 years ago. Further investigations are needed to better understand paleoseismic activity and long-term seismic risk of the Kamishiro fault.</p>

    DOI： 10.11462/afr.2015.43_109

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  • Surface rupture of the 2014 Kamishiro fault earthquake

    Hirouchi Daisuke, Sugito Nobuhiko, Kaneda Heitaro, Goto Hideaki, Matsuta Nobuhisa, Suzuki Yasuhiro

    Proceedings of the General Meeting of the Association of Japanese Geographers   2015 ( 87 )   100278 - 100278   2015

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    DOI： 10.14866/ajg.2015s.0_100278

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  • Surface rupture associated with the 2014 Naganoken-hokubu earthquake (Kamishiro fault earthquake), central Japan

    Hirouchi Daisuke, Suzuki Yasuhiro, Watanabe Mitsuhisa, Sawa Hiroshi, Miyauchi Takahiro, Forteenth Year Kamishiro Fault Earthquake Research Group for the Twenty-, Matsuta Nobuhisa, Sugito Nobuhiko, Kumahara Yasuhiro, Ishiguro Satoshi, Kaneda Heitaro, Goto Hideaki, Kagohara Kyoko, Nakata Takashi

    Active Fault Research   2015 ( 43 )   149 - 162   2015

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    Language：Japanese   Publisher：Japanese Society for Active Fault Studies  

    <p>The 2014 M 6.7 Naganoken-hokubu earthquake was caused by movement of the Kamishiro fault located in the northernmost part of the Itoigawa-Shizuoka Tectonic Line (ISTL) active fault system, central Japan. We conducted a series of field research immediately after the earthquake to describe coseismic surface ruptures. Our description methods were: 1) field reconnaissance using pre- and post-earthquake airphotos; 2) quick measurement using staff; 3) topographic profiling using Auto Level and Total Station; and, 4) UAV and highpole SfM measurement. We identified 9-km-long coseismic surface rupture, most of which was located along the pre-existing surface trace of the Kamishiro fault. The maximum value of coseismic vertical offset was ca. 1 m or more, which was recorded at Oide in the northern part of the rupture. Based on comparison of the 2014 coseismic slip distribution with the long-term slip rate distribution, both 2014 slip amount and cumulative offset amounts of L2 and L3 terrace surfaces are larger in the northern end of the ruptures. This implies that the subsurface coseismic slip during pre-2014 earthquakes continued toward the north, similar to that during the 2014 earthquake. In addition, both coseismic slip and long-term slip rate becomes smaller toward the south, indicating that the Kamishiro area is one of the segment boundaries in the northern part of the ISTL active fault system. Further investigations of the 2014 earthquake and the Kamishiro fault are needed to understand formation of tectonic landforms, landscape development, or earthquake prediction model of active faults.</p>

    DOI： 10.11462/afr.2015.43_149

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  • What Differentiated Local Casualties Caused by the Tsunami ?

    TAKAHASHI Makoto, MATSUTA Nobuhisa

    Journal of Geography (Chigaku Zasshi)   124 ( 2 )   193 - 209   2015

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    Language：Japanese   Publisher：Tokyo Geographical Society  

    &emsp;Generally, the impacts of a tsunami can be understood in terms of the corresponding relationships between hazard scale and extent of building damage and loss of human life. Focusing on community-scale statistics of the municipalities of Kamaishi, Kesen'numa, Minami-sanriku, and Yamamoto, which were severely affected by the 2011 Tohoku Earthquake, significant variations are observed in the mortality rates at affected villages that experienced the same levels of building damage. Moreover, differences in the geographical locations of the villages also impact their mortality rates. A village with a high mortality rate is situated either on a coastal plain or on an inland valley plain some distance from the sea, whereas a village with a low mortality rate is paradoxically in close proximity to the sea, often facing a small bay. Close interrelationships are identified among geographical conditions and possible evacuation activities, which relate to the geographical imaginations of inhabitants based on their inherent local knowledge and interactions with physical and built environments. Interviews with survivors indicate decisions to escape could not be made quickly after the earthquake occurred. Rather, people were confused regarding the occurrence and magnitude of the tsunami and the provision of evacuation sites. The tsunami waves were often different from those that were formally forecast and broadcast, which compelled people to act flexibly. Consequently, it is argued that it is necessary to emphasize the effects of local geographies on interactions between tsunami waves and evacuation activities from a grassroots perspective when preparing for future tsunamis.

    DOI： 10.5026/jgeography.124.193

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  • Source Fault Model of the 2011 off the Pacific Coast of Tohoku Earthquake, Estimated from the Detailed Distribution of Tsunami Run-up Heights

    MATSUTA Nobuhisa, SUZUKI Yasuhiro, SUGITO Nobuhiko, NAKATA Takashi, WATANABE Mitsuhisa

    Journal of Geography (Chigaku Zasshi)   124 ( 2 )   177 - 192   2015

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    Language：Japanese   Publisher：Tokyo Geographical Society  

    &emsp;The distribution of tsunami run-up heights generally has spatial variations, because run-up heights are controlled by coastal topography including local-scale landforms such as natural levees, in addition to land use. Focusing on relationships among coastal topography, land conditions, and tsunami run-up heights of historical tsunamis&mdash;Meiji Sanriku (1896 A.D.), Syowa Sanriku (1933 A.D.), and Chilean Sanriku (1960 A.D.) tsunamis&mdash;along the Sanriku coast, it is found that the wavelength of a tsunami determines inundation areas as well as run-up heights. Small bays facing the Pacific Ocean are sensitive to short wavelength tsunamis, and large bays are sensitive to long wavelength tsunamis. The tsunami observed off Kamaishi during the 2011 off the Pacific coast of Tohoku Earthquake was composed of both short and long wavelength components. We examined run-up heights of the Tohoku tsunami, and found that: (1) coastal areas north of Kamaishi and south of Yamamoto were mainly attacked by short wavelength tsunamis; and (2) no evidence of short wavelength tsunamis was observed from Ofunato to the Oshika Peninsula. This observation coincides with the geomorphologically proposed source fault model, and indicates that the extraordinary large slip along the shallow part of the plate boundary off Sendai, proposed by seismological and geodesic analyses, is not needed to explain the run-up heights of the Tohoku tsunami. To better understand spatial variations of tsunami run-up heights, submarine crustal movements, and source faults, a detailed analysis is required of coastal topography, land conditions, and submarine tectonic landforms from the perspective of geomorphology.

    DOI： 10.5026/jgeography.124.177

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  • The toll of the victims of the Mikawa earthquake by the surface rupture along the Fukozu fault

    Matsuta Nobuhisa, Kimata Fumiaki

    Proceedings of the General Meeting of the Association of Japanese Geographers   2015 ( 87 )   100231 - 100231   2015

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    Publisher：The Association of Japanese Geographers  

    This study was analyzed building damage and human damages by the 1944 Tonankai earthquake and the Mikawa earthquake in Aichi Prefecture. We compared in detail the number of collapse house, victims, and physical geographic condition, at the village scale. As the result we can show the feature of disaster type by the earthquake shock and the displacement. On the earthquake shock, houses are destroyed. Since it takes time to be completely destroyed, people has the time to escape from the onslaught of violence. On the other hand, on the displacement houses are destroyed in a moment before people escape.

    DOI： 10.14866/ajg.2015s.0_100231

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  • Spatial Variations of Tsunami Run-up Heights for the 2011 off the Pacific Coast of Tohoku Earthquake, Based on GIS Analysis of Tsunami Inundation Area Data and Digital Elevation Model

    SUGITO Nobuhiko, MATSUTA Nobuhisa, ISHIGURO Satoshi, UCHIDA Chikara, SENDA Yoshimichi, SUZUKI Yasuhiro

    Journal of Geography (Chigaku Zasshi)   124 ( 2 )   157 - 176   2015

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    Language：Japanese   Publisher：Tokyo Geographical Society  

    &emsp;Spatial variations of hazards such as strong ground motion and tsunami inundation are a key element for obtaining a geographical understanding of natural disasters. However, detailed distribution of tsunami run-up heights for the devastating tsunami associated with the 2011 off the Pacific coast of Tohoku earthquake is not available. A GIS analysis of tsunami inundation areas is conducted from data collected by the Tsunami Damage Mapping Team and from post-tsunami 2-m mesh and 5-m mesh digital elevation models (DEM) after the Geospatial Information Authority of Japan, in order to produce the Tsunami Run-up Height Map, which includes polygon data of inundation areas with elevation data at each point. Horizontal shifts of orthophotos taken just after the tsunami are corrected using a Helmert transformation. The map covers Iwate Prefecture, Miyagi Prefecture, and the northern part of Fukushima Prefecture continuously at high resolutions, and reveals spatial variations of tsunami run-up heights in detail. These variations are caused by: 1) landforms at each site, such as coastal plains, valleys, bays, and beach ridges, as well as their directions and magnitudes, and 2) source locations, interference, and wavelengths of the tsunami, as implied by a previous study. The map supports examination carried out on source fault models and simulation results of tsunamis from a geographical viewpoint. At the same time, the methodology to produce the map would be useful for systematically revealing run-up height distribution, in addition to inundation areas immediately after future tsunamis.

    DOI： 10.5026/jgeography.124.157

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  • Active fault along the Kamishiro fault, Central Japan, Especially its close coincidence with the location of the surface rupture associated with the 2014 Kamishiro fault earthquake

    SAWA Hiroshi, MATSUTA Nobuhisa, WATANABE Mitsuhisa, SUZUKI Yasuhiro, NAKATA Takashi

    Proceedings of the General Meeting of the Association of Japanese Geographers   2015 ( 87 )   100208 - 100208   2015

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    DOI： 10.14866/ajg.2015s.0_100208

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  • Pictorial 1: Tsunami Run-up Height Map for the 2011 Pacific Coast of Tohoku Earthquake around Motoyoshi-cho, Kesen-numa City, Miyagi Prefecture

    SUGITO Nobuhiko, MATSUTA Nobuhisa, ISHIGURO Satoshi, UCHIDA Chikara, SANO Shigeki, SENDA Yoshimichi, SUZUKI Yasuhiro

    Journal of Geography (Chigaku Zasshi)   124 ( 2 )   vii - vii   2015

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    Language：Japanese   Publisher：Tokyo Geographical Society  

    DOI： 10.5026/jgeography.124.vii

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  • Pictorial 4: Anaglyph Images Using Aerial Photographs Taken Just after the 2011 Pacific Coast of Tohoku Earthquake

    SUZUKI Yasuhiro, MATSUTA Nobuhisa, SUGITO Nobuhiko

    Journal of Geography (Chigaku Zasshi)   124 ( 2 )   x - x   2015

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    Language：Japanese   Publisher：Tokyo Geographical Society  

    DOI： 10.5026/jgeography.124.x

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  • 2014年長野県北部の地震(神城断層地震)に伴う地表地震断層と活断層

    廣内大助, 杉戸信彦, 金田平太郎, 後藤秀昭, 松多信尚, 鈴木康弘, 石黒聡士, 熊原康博

    日本地球惑星科学連合大会予稿集(Web)   2015   2015

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  • 1944年東南海地震の被害再検討(1)戦禍がもたらした震災

    木股文昭, 木股文昭, 松多信尚

    歴史地震(Web)   ( 30 )   2015

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  • 三河地震における死亡者と活断層および地形との関係

    松多信尚, 木股文昭, 木股文昭

    歴史地震(Web)   ( 30 )   2015

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  • 2014年長野県北部の地震(神城断層地震)で現れた地表地震断層と既存活断層の位置関係

    澤祥, 松多信尚, 渡辺満久, 鈴木康弘, 中田高

    日本地球惑星科学連合大会予稿集(Web)   2015   2015

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  • 災害と共存して生きていくための観光防災街歩き地図-幸田町での試み-

    山中佳子, 松多信尚, 小川真護, 小川真護, 近藤ひろ子, 近藤ひろ子, 遠藤悠, 中井春香

    日本地球惑星科学連合大会予稿集(Web)   2015   2015

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  • A method for measuring surface rupture displacement by using UAV-Application to the 2014 Kamishiro fault earthquake

    ISHIGURO Satoshi, KUMAHARA Yasuhiro, NAKATA Takashi, GOTO Hideaki, WATANABE Mitsuhisa, MIYAUCHI Takahiro, KAGOHARA Kyoko, SUGITO Nobuhiko, MATSUTA Nobuhisa, HIROUCHI Daisuke

    日本地球惑星科学連合大会予稿集(Web)   2015   2015

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  • Field evidence of tsunami sediments along the east coast of Taiwan

    NISHIKAWA Yuka, CHEN Wen-shan, YEN Jiun-yee, MATSUTA Nobuhisa, YU Neng-ti

    日本地球惑星科学連合大会予稿集(Web)   2015   2015

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  • Ground surface deformation of small mud volcano by repeated measurements of terrestrial laser scanning (Murono, Japan)

    HAYAKAWA Yuichi S., KUSUMOTO Shigekazu, MATSUTA Nobuhisa

    日本地球惑星科学連合大会予稿集(Web)   2015   2015

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  • 1891年濃尾地震災害の再検討(2)全家屋全潰の地域

    木股文昭, 松多信尚

    日本地震学会秋季大会講演予稿集   2014   2014

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  • Shallow seismic reflection profiles in Saga plain

    Kagohara Kyoko, Okada Shinsuke, Matsuta Nobuhisa, Toda Shigeru, Soeda Yoshio, Imaizumi Toshifumi

    Proceedings of the General Meeting of the Association of Japanese Geographers   2014 ( 86 )   53 - 53   2014

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    Publisher：The Association of Japanese Geographers  

    DOI： 10.14866/ajg.2014a.0_53

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  • Late Pleistocene and Holocene Faulting of the Central Part of the Atera Fault Zone in the Futawatari area, Eastern part of Gifu Prefecture, Central Japan

    Hirouchi Daisuke, Yasue Ken-ichi, Doke Ryosuke, Sato Yoshiki, Sugito Nobuhiko, Matsuta Nobuhisa

    Annual Meeting of the Geological Society of Japan   2014   594 - 594   2014

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    Publisher：The Geological Society of Japan  

    DOI： 10.14863/geosocabst.2014.0_594

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  • Takahashi, M., Tanaka, S. and Kimata, F. eds.: Tsunami Disaster and Reconstruction in Aceh Following the 2004 Sumatra Earthquake

    Nobuhisa MATSUTA

    Geographical review of Japan series A   87 ( 5 )   421 - 422   2014

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    Language：Japanese   Publisher：The Association of Japanese Geographers  

    DOI： 10.4157/grj.87.421

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  • An Acceleration Event of Creeping Slip Detected by Precise Leveling Survey at the Central Part of the Longitudinal Valley Fault, Eastern Taiwan (2010-2013)

    ( 49 )   231 - 242   2014

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  • An Acceleration Event of Creeping Slip Detected by Precise Leveling Survey at the Central Part of the Longitudinal Valley Fault, Eastern Taiwan (2010-2013)

    村瀬雅之, 松多信尚, LIN Cheng-Hong, CHEN Wen-Shan, LIN Jui-Jen, 西川由香, 和田絵里香, 小泉尚嗣

    日本大学文理学部自然科学研究所研究紀要   ( 49 )   231 - 242   2014

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  • Knickpoint Recession Rates for 10 Years after the Chi-Chi Earthquake, Central Taiwan

    HAYAKAWA Yuichi S., MATSUTA Nobuhisa, MAEKADO Akira, MATSUKURA Yukinori

    地形   34 ( 1 )   21 - 36   2013.1

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    Language：Japanese  

    Recession rates of four waterfalls formed by the surface deformation of the Chelungpu Fault at the time of Chi-Chi Earthquake on September 21, 1999 in central Taiwan were measured in the field and assessed with an empirical model of waterfall erosion. The model represents the balance between the erosive force of streams versus bedrock resistance with relevant environmental parameters of discharge (drainage area and precipitation), waterfall form and bedrock strength. The recession rates of three waterfalls increased from the first 6 years to the following 4 years. This increase in the recession rates basically corresponds to the changes in environmental factors including precipitation increase and waterfall width narrowing. The recession rate of another waterfall decreased, but this can be explained by artificial modification of riverbed. The recession rates are very high comparing with waterfalls in other places, probably due to large amount of hard gravels transported on the weak bedrock from the upstream areas.

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    Other Link： http://dl.ndl.go.jp/info:ndljp/pid/10808629

  • P3. Downcutting of the Daan River around uplifted area in Taiwan(Fall Meeting of the Union, September 2012)

    MATTA Nobuhisa, ISHIGURO Satoshi, HAYAKAWA Yuichi S., CHEN Wenshan

    34 ( 1 )   82 - 82   2013

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  • An episodic creep-slip event detected by precise levelling surveys in the central part of the Longitudinal Valley Fault, eastern Taiwan, in 2011-2012

    MURASE Masayuki, MATTA Nobuhisa, LIN Cheng-Hong, CHEN Wen-Shan, KOIZUMI Naoji

    Tectonophysics   608   904 - 913   2013

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    Language：English   Publisher：ELSEVIER SCIENCE BV  

    Precise levelling surveys were conducted across the central Longitudinal Valley Fault, eastern Taiwan, to understand the deformation of the transition zone between the stable fault creep area and the asperity area. In order to investigate the surface relationship between the fault creep area and the geological condition of the transition zone, we established levelling routes in the Yuli, Chike-san, and Reishuei areas. The Yuli area forms the geological boundary of the Lichi Melange Formation, which is composed of chaotic mudstones containing numerous exotic blocks of various sizes and lithologies. Along the Yuli route, located on the Lichi Melange, an uplift rate of 30 mm/yr was detected during the period 2010-2012, suggesting that aseismic fault creep might be continuing with long-term stability. Along the Chike-san route, a vertical deformation rate of 8 mm/yr was detected in the period 2010-2011. However, a large deformation with an uplift rate of 40 mm/yr was detected in the period 2011-2012. Along the Reisuei route, we detected a deformation of 8 mm/yr in the period 2011-2012.A two-dimensional single-fault model was developed to discuss the slip distributions in the periods 2010-2011 and 2011-2012. Relatively large slip rates were estimated at two parts of the fault plane one at a depth of similar to 1.5 km and another at a depth of similar to 4 km in both periods. Because both parts of the fault plane show approximately the same slip distribution, we believe that the detected deformation resulted from an episodic acceleration event of creeping slip.The northern limit of the stable creep area may be the Yuli area. The episodic creep event occurred in the transition zone between the stable fault creep area and the asperity area. The boundary between the stable creep area and the episodic creep area is consistent with the geological boundary of the Lichi Melange Formation. (C) 2013 Elsevier B.V. All rights reserved.

    DOI： 10.1016/j.tecto.2013.07.027

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  • Finding of Probable Tsunami Boulders on Jiupeng Coast in Southeastern Taiwan

    Nobuhisa Matta, Yoko Ota, Wen-Shan Chen, Yuka Nishikawa, Masataka Ando, Ling-Ho Chung

    TERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES   24 ( 1 )   159 - 163   2013

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    Language：English   Publisher：CHINESE GEOSCIENCE UNION  

    We find three coral boulders (approx. 5 m across) resting on the Holocene coral terrace on the Jiupeng coast of southeastern Taiwan. Three exotic corals on the outer part of the boulders are dated at ca. 5000 yr BP which is similar to that of in situ corals composing the Holocene terrace. We interpret that these boulders were broken off from the coral terrace and were transported by tsunami waves, although the timing of the paleotsunami is not determined at this stage.

    DOI： 10.3319/TAO.2012.09.14.01(TT)

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  • Spatial variation of runup height of the tsunami associated with the 2011 off the Pacific coast of Tohoku earthquake, revealed by GIS-based analysis of tsunami-damage map and DEM

    SUGITO Nobuhiko, MATSUTA Nobuhisa, ISHIGURO Satoshi, UCHIDA Chikara, SENDA Yoshimichi, SUZUKI Yasuhiro

    Proceedings of the General Meeting of the Association of Japanese Geographers   2013 ( 84 )   100022 - 100022   2013

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    Publisher：The Association of Japanese Geographers  

    DOI： 10.14866/ajg.2013a.0_100022

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  • The Feature of Thunami Height Categorized by Coastal Landform, Comparison of Meiji Sanriku Tsunami with the 2011 off the Pacific Coast of Tohoku Earthquake Tsunami, Japan

    Matsuta Nobuhisa

    Proceedings of the General Meeting of the Association of Japanese Geographers   2013 ( 83 )   128 - 128   2013

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    Publisher：The Association of Japanese Geographers  

    DOI： 10.14866/ajg.2013s.0_128

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  • Difference of the tsunami height according to type of the coastal landforms in the case of the 2011 Tohoku-oki tsunami and historical tsunamis

    MATSUTA Nobuhisa, SUGITO Nobuhiko, SENDA Yoshimichi, HORI Kazuaki, ISHIGURO Satoshi, UCHIDA Chikara, SUZUKI Yasuhiro

    Proceedings of the General Meeting of the Association of Japanese Geographers   2013 ( 84 )   100091 - 100091   2013

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    DOI： 10.14866/ajg.2013a.0_100091

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  • 航空写真を用いた東北地方太平洋沖地震の津波遡上高分布

    鈴木康弘, 石黒聡士, 杉戸信彦, 松多信尚, 内田主税

    土木計画学研究・講演集(CD-ROM)   47   2013

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  • Surface deformation caused by the northern part of Nagano earthquake

    9 - 15   2012.1

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  • Large Aseismic Creep Detected by Precise Leveling Survey at the Central Part of the Longitudinal Valley Fault, Southeast Taiwan (2008-2011)

    村瀬雅之, 松多信尚, 小澤和浩, LIN Cheng-Hong, CHEN Wen-Shan, LIN Jui-Jen

    日本大学文理学部自然科学研究所研究紀要   ( 47 )   241 - 254   2012

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  • Criteria for Detection of Tsunami-inundation Area Associated with the 2011 off the Pacific Coast of Tohoku Earthquake, Northeast Japan, Based on Air-photo Stereo-pair Interpretation

    杉戸信彦, 松多信尚, 後藤秀昭, 熊原康博, 堀和明, 廣内大助, 石黒聡士, 中田高, 海津正倫, 渡辺満久, 鈴木康弘

    自然災害科学   31 ( 2 )   113 - 125   2012

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  • Large Aseismic Creep Detected by Precise Leveling Survey at the Central Part of the Longitudinal Valley Fault, Southeast Taiwan (2008-2011)

    ( 47 )   241 - 254   2012

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  • P8. Uplift of the Matsudai mud volcano associated with the earthquake near the border of Nagano and Niigata Prefectures, measured by 3D laser scanner(Abstracts of Paper Presented at Fall Meeting of the Union, September 2011)

    MATTA Nobuhisa, HAYAKAWA Yuichi S., HORI Kazuaki, KUO Yu-ting, SUGITO Nobuhiko

    33 ( 1 )   94 - 95   2012

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  • What the causes of differentiated local casualties in the 2011 Tohoku Earthquake?

    Takahashi Makoto, Hori Kazuaki, Matsuta Nobuhisa, Tanaka Shigeyoshi

    Proceedings of the General Meeting of the Association of Japanese Geographers   2012 ( 82 )   100058 - 100058   2012

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    Publisher：The Association of Japanese Geographers  

    In this paper, we examine the interrelationships between locally varied casualties, and physical mechanisms of tsunami flows, physical geographies and social conditions of the localities, and then discuss what caused the catastrophe in the 2011 Tohoku Earthquake.

    DOI： 10.14866/ajg.2012a.0_100058

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  • Significance and Background of Mapping the Area Hit by the Tsunami on March 11, 2011, Northeast Japan

    松多信尚, 杉戸信彦, 後藤秀昭, 石黒聡士, 中田高, 渡辺満久, 宇根寛, 田村賢哉, 熊原康博, 堀和明, 廣内大助, 海津正倫, 海津正倫, 碓井照子, 鈴木康弘

    E-journal GEO   7 ( 2 )   214 - 224   2012

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    Language：Japanese   Publisher：The Association of Japanese Geographers  

    The March 11, 2011, earthquake off the Pacific coast of northeastern Japan caused large tsunami. Tsunami-damaged areas were mapped on a scale of 1 : 25,000 based on the interpretation of stereopaired aerial photographs taken immediately after the earthquake by the Geospatial Information Authority of Japan. The area interpreted in this study was from Aomori to Chiba prefecture, except for the restricted area around the Fukushima nuclear power plant. Areas for which no aerial photographs were available were mapped using Google Earth and other sources. The purpose of mapping was to provide prompt basic information on the extent of tsunami invasion and distribution of devastated areas for all people taking countermeasures against the disaster. The lessons from our mapping area are that 1) aerial photographs should be taken as soon as possible after disasters and 2) a working team should be quickly arranged to map damaged areas and release the results.

    DOI： 10.4157/ejgeo.7.214

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  • 1:25,000-Scale Tsunami-Damage Map on the 2011 off the Pacific Coast of Tohoku Earthquake, Japan, Based on Airphoto Interpretation

    Association of Japanese Geographers Tsunami Damage Mapping Team, Matsuta Nobuhisa

    Proceedings of the General Meeting of the Association of Japanese Geographers   2012 ( 81 )   100262 - 100262   2012

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    Japanese only

    DOI： 10.14866/ajg.2012s.0_100262

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  • Course change of the Isuzu River caused by a giant tsunami in the southern part of the Ise Plain

    MATSUTA nobuhisa, SUGITO Nobuhiko, OKUNO Naoyuki

    Proceedings of the General Meeting of the Association of Japanese Geographers   2012 ( 82 )   100153 - 100153   2012

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    Focusing on the river-course change of the Isuzu river, we suppose the event was caused by the giant tsunami. We found the evidence in alluvial plain by Geo-slicer.

    DOI： 10.14866/ajg.2012a.0_100153

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  • 塩野原基線の再測量

    鷺谷威, 鷺谷威, 太田雄策, 松多信尚, MENESES Angela, 野村晋一, 鈴木翔太

    日本測地学会講演会要旨   118th   2012

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  • 津波被災地における名古屋大グループの浸水高調査 (特集 東日本大震災地震と津波・地盤災害)

    海津 正倫, 杉戸 信彦, 松多 信尚

    地理   56 ( 12 )   38 - 45   2011.12

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  • 地形学は東北地方太平洋沖地震を予測できたのか (緊急特集 東日本大震災)

    松多 信尚

    地理   56 ( 6 )   83 - 89   2011.6

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  • 水準測量で検出された台東縦谷断層中部の大規模クリープ現象2011(速報)

    村瀬雅之, 松多信尚, LIN Jui-Jen, CHEN Wen-shan, LIN Cheg-Horng

    日本測地学会講演会要旨   116th   2011

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  • Creep deformation upon the Yuli Fault in the Taiwan Longitudal Valley: Deformation of the Yuli Bridge

    Kawabata Kuniyo, Matsuta Nobuhisa, Ando Masataka, Asai Yasuhiro, Koizumi Naoji, Tasaka Shigeki, Tsunomori Fumiaki, Nakamura Mamoru, Lai Wen-Chi

    The Journal of the Geological Society of Japan   117 ( 1 )   I - II   2011

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    Language：Japanese   Publisher：The Geological Society of Japan  

    DOI： 10.5575/geosoc.117.1.I_II

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  • Creeping deformation for 30 years along the Longitudinal Valley fault

    Matta Nobuhisa, Ishiguro Satoshi, Murase Masayuki, Chen Wen-shan

    Proceedings of the General Meeting of the Association of Japanese Geographers   2011 ( 79 )   247 - 247   2011

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    DOI： 10.14866/ajg.2011s.0.247.0

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  • 2011年3月12日長野県・新潟県県境付近の地震に伴う地表変状 (速報)

    松多信尚

    http://www.ajg.or.jp/disaster/files/201103_Nagano-Niigata_eq.pdf   2011

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  • Preservation of the active fault that caused the 921 earthquake in Chichi, Taiwan and its process

    Bulletin of the National Museum of Japanese History   156   7 - 37[含 英語文要旨]   2010.3

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  • Paleoearthquake activity in late Holocene time in the Luyeh fault in the Longitudinal valley system, eastern Taiwan

    Matsuta Nobuhisa, Chen W. S., Chi C.Y., Yang C., Huang N.W., for the Luyeh fault Tectonic Paleoseismology Research Group

    Proceedings of the General Meeting of the Association of Japanese Geographers   2010 ( 77 )   247 - 247   2010

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    DOI： 10.14866/ajg.2010s.0.247.0

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  • Possible evidences for paleotsunami along the east coast of Taiwan

    Matta Nobuhisa, Ota Yoko, Ando Masataka, Haraguchi Tsuyoshi, Nishikawa Yuka, Switzer Adam, LIN Cheng-Horng

    Proceedings of the General Meeting of the Association of Japanese Geographers   2010 ( 78 )   88 - 88   2010

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    Paleotsunami is one of the indicators for reconstruction of paleoearthquakes. It has been generally considered that the east coast of Taiwan has not been affected by large tsunami, due to the absence of documented records in the short historical time, and also due to steep offshore submarine morphology. A legend of the Ami tribe says, however, that strong waves have rushed toward the northern part of the east coast.In addition, a local historian tells a story that a sudden disappearance of vegetation has occurred at Chenggong town at ca. 150 years ago. We infer that this environmental change may record a tsunami event on this coast and wish to confirm the occurrence of tsunami by excavation of Holocene deposits. The excavated sites are located on the lower Holocene marine terraces at 15-20 m asl at Chenggong area. The first excavation was done by hand-augering on Sept. 2009, and the second one was by using Geoslicer at four sites on March, 2010. In addition, we have observed coastal feature along the east coast of Honchuan Peninsula. This preliminary report provides two lines of geological evidences for possible tsunami origin. One is the presence of two abrupt facies changes from terrestrial condition to marine or brackish condition, event I and II, at Site 1. Available radiocarbon date suggests the event I occurred at 1850 to 1600 cal yr BP, thus event II is further younger than this age. We are working on various kinds of analysis, including radiocarbon dating, to confirm the tsunami origin for observed features.

    DOI： 10.14866/ajg.2010f.0.88.0

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  • Prediction of coseismic fault behavior based on slip-rate and slip distributions for the northern part of the Itoigawa-Shizuoka Tectonic Line active fault zone, central Japan

    Suzuki Yasuhiro, Ishiguro Satoshi, Sato Yoshiki, Sugito Nobuhiko, Kumamoto Takashi, Sawa Hiroshi, Watanabe Mitsuhisa, Matsuta Nobuhisa, Hirouchi Daisuke, Taniguchi Kaoru, Tajikara Masayoshi

    Active Fault Research   2010 ( 33 )   1 - 14   2010

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    Language：Japanese   Publisher：Japanese Society for Active Fault Studies  

    The Itoigawa-Shizuoka Tectonic Line active fault zone is one of the largest active faults in Japan, with a length of 150 km. The previous paleoseismological studies revealed a 14% possibility of a large earthquake in the next 30 years. The Japanese Ministry of Education, Culture, Sports, Science and Technology has initiated an intensive research project on this fault zone in 2005, in which we have conducted a tectonic geomorphological study on the northern part of the fault zone in order to predict its coseismic behavior. We have interpreted largescale aerial photographs taken not only in recent years but also in the 1940s and 1960s for examining faultrelated topography including those which have been already modified or destroyed, and then conducted a field survey to determine ages of geomorphic surfaces. We also carried out photogrammetric analyses which have resulted in our highly-dense offset data whose spatial intervals are of 500-1000 meters in average. Based on these surveys, we estimated a net-slip rate distribution along the northern part of the fault zone, and calculated coseismic slip distribution assuming that the fault zone follows the characteristic earthquake model. Largeroffset areas were identified in the Hakuba Village and the Ikeda Town. These peaks of surficial slip distribution would imply subsurface fault which generate strong ground motion. The maximum vertical offset during the last earthquake is estimated to be 5 - 6 meters. Therefore, the coseismic net slip would exeed 10 meters when we assume the fault-slip responds to the maximum shear stress. Our detailed coseismic slip distribution and the subsurface fault geometry predict a moment magnitude of 7.5 for the northern part of the fault zone.

    DOI： 10.11462/afr.2010.33_1

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  • Rapid Recession of Fault-scarp Waterfalls : Six-year Changes Following the 921 Chi-Chi Earthquake in Taiwan

    HAYAKAWA Yuichi S., MATSUTA Nobuhisa, MATSUKURA Yukinori

    Transactions,Japanese Geomorphological Union   30 ( 1 )   1 - 13   2009.1

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    Recession of waterfalls is a significant agent in bedrock river erosion and development, but field data on waterfall recession rates have been limited due mainly to the lack of information on initiation age and recession distance of waterfalls. This study examines recession rates of fault-scarp waterfalls that were formed along the Chelungpu surface fault at the 921 Chi-Chi Earthquake on September 21, 1999 at central Taiwan. Our field measurements reveal the 6-year mean recession rate of the waterfalls to be 3.3-58.2m/y, which is considerably higher than any other waterfall recession rate in the world. In order to explore the factors affecting the observed high waterfall recession rate, relationships between the waterfall recession rate and relevant physical parameters (comprising erosive force and bedrock resistance) are examined using a previously proposed empirical model. Applying field measured parameters at the rivers, the previously established equation provides an estimated recession rate of 0.6-3.9m/y, which is much lower than the actual recession rate. The discrepancy between the actual and equation-derived recession rates is likely due to abundant abrasive material in the rivers, which may considerably enhance waterfall recession.

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    Other Link： http://dl.ndl.go.jp/info:ndljp/pid/10808011

  • Web-GIS Based Active Fault Information System for the Itoigawa-Shizuoka Tectonic Line

    SUZUKI Yasuhiro, TANIGUCHI Kaoru, SUGITO Nobuhiko, SAKAUE Hiroyuki, UCHIDA Chikara, WATANABE Mitsuhisa, SAWA Hiroshi, MATSUTA Nobuhisa, TAJIKARA Masayoshi, HIROUCHI Daisuke

    E-journal GEO   4 ( 1 )   37 - 46   2009

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    The geographical information with regard to active faults (for example; precise location, cumulative amount and shape of deformation, and slip-rate) is compiled on the &ldquo;Web-GIS based active fault information system for the Itoi-gawa-Shizuoka Tectonic Line&rdquo;. This can be a compilation of the basic information not only for earthquake anticipa-tion, but also for land use planning in order to mitigate earthquake disaster. These fundamental data and visual graphics illustrating the relation between active faults and tectonic landforms are compiled on the system, which became opened for public. We are here presenting methodology for constituting the system as an effected hazard map toward disaster mitigation. Tectonic geomorphological survey of the northern and middle Itoigawa-Shizuoka Tectonic Line was conducted and it clarifies the detailed distribution of the slip-rates of the fault. That would enable us to forecast the behavior of the fault and to estimate the strong ground motion associated with an earthquake. Fur-thermore, the digital elevation model with high density and high precision was constructed photogrammetrically by using 1:15,000 scale aerial photographs. The aerial photographs taken in the 1940s or 1960s were also used in areas where tectonic landforms had already been artificially modified; this was intended to reconstruct the original land-forms. The landform deformations by faulting were analyzed densely from many transactions that were measured under the photogrammetrical system.

    DOI： 10.4157/ejgeo.4.37

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  • The Comparative Study of Earthquake Memory and Transference-Case Studies of Turkey, Taiwan and Indonesia-

    阪本真由美, 木村周平, 松多信尚, 松岡格, 矢守克也

    京都大学防災研究所年報(CD-ROM)   ( 52 )   181 - 194   2009

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    Language：Japanese   Publisher：Disaster Prevention Research Institute Kyoto University  

    The memories of past disaster experiences tend to fade out quickly. Survivors do not want to keep horrible memories, and try to forget it. Although the transference of lessons learnt through past disaster experience is considered as one of ways to motivate people to take disaster preventive action, the mechanism of how the personal memory form collective memory and transfer to other generation/region is still not clear. In this study, we focus on the memory of earthquake disaster in different region, Turkey, Taiwan and Indonesia. Through field studies we try to find out what kind of memory do people talk as personal memory, and how those personal memory form collective memory and will be transferred.

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    Other Link： http://hdl.handle.net/2433/129329

  • Precise leveling survey at the Yuli fault, Southeast Taiwan

    村瀬雅之, 松多信尚, LIN Jui-Jen, PU Hsin-Chieh, CHEN Wen-Shan, LIN Cheng-Hong

    Proceedings of the Institute of Natural Sciences, Nihon University   ( 44 )   159 - 166   2009

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  • The 1999 earthquake fault and its repeated occurrence at the Earthquake Museum of Taiwan, central part of the Chelungpu Fault

    Ota Yoko, Matsuta Nobuhisa

    Active Fault Research   2009 ( 31 )   33 - 38   2009

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    The Chelungpu Fault, Taiwan, records the surface rupture by the 1999 Chichi earthquake and abundant information has been obtained on paleoseismology on this fault during the last 10 years. This study area, located on the central part of the Chelungpu Fault, is known as one of the type localities of the surface rupture, but no paleoseismological study was carried out. This paper reports the trench log across the Chelungpu Fault preserved at the Earthquake Museum of Taiwan and tries to reconstruct the faulting history at this site based on 10 bore hole data on the location of the museum. Trench log indicates the displacement of terrace deposits and underlying bedrock by the 1999 earthquake. Four subparallel faults are observed within 1.8 m width, corresponding to the location of the surface rupture. Estimated height difference of bedrock surface based on the bedrock height by bore hole data is more than 4.2 m, significantly larger than the offset by the 1999 earthquake (2-2.5 m). This fact implies that at least two earthquake events including the 921 earthquake occurred at this site. We also estimate the fault plane dips eastward at about 30 degree, based on the location and stratigraphy of one bore hole which penetrates to the terrace gravel on the footwall through the bedrock.

    DOI： 10.11462/afr.2009.31_33

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  • Precise leveling survey at the Yuli fault, southeast Taiwan

    Proceedings of the Institute of Natural Sciences Nihon University Department of geosystem sciences   ( 44 )   159 - 166   2009

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  • Study of tectonic landforms and late Quaternary slip rates along the middle part of the Itoigawa-Shizuoka Tectonic Line active fault system, central Japan

    SAWA Hiroshi, MATSUTA Nobuhisa, SUGITO Nobuhiko, Tectonic Geomorphological Research Group for ISTL Active fault System

    Proceedings of the General Meeting of the Association of Japanese Geographers   2008 ( 73 )   172 - 172   2008

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    Language：Japanese   Publisher：The Association of Japanese Geographers  

    DOI： 10.14866/ajg.2008s.0.172.0

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  • Preservation of the Chelungpu fault in Taiwan

    MATSUTA Nobuhisa, NISHIKAWA Yuka

    Proceedings of the General Meeting of the Association of Japanese Geographers   2008 ( 73 )   203 - 203   2008

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    Language：Japanese   Publisher：The Association of Japanese Geographers  

    DOI： 10.14866/ajg.2008s.0.203.0

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  • Subsurface fault geometry and slip direction from Chino to Hakushu in the central to southern portion of the ISTL active fault system, central Japan, based on detailed analysis of tectonic landform

    SUGITO Nobuhiko, MATSUTA Nobuhisa, SAWA Hiroshi, ISTL Active Fault System Tectonic Geomorphological Research Group for

    Proceedings of the General Meeting of the Association of Japanese Geographers   2008 ( 73 )   123 - 123   2008

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    DOI： 10.14866/ajg.2008s.0.123.0

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  • Tectonic geomorphology and slip rates along a frontal thrust (the Changhua fault), middle western Taiwan organic belt

    MATSUTA Nobuhisa, Chen Wen-Shan, Yu Neng-Ti, Shih Ruey-Chyuan, Yang Chih-Cheng, for the Changhua fault Tectonic Geomorphological Research Group

    Proceedings of the General Meeting of the Association of Japanese Geographers   2008 ( 73 )   124 - 124   2008

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    DOI： 10.14866/ajg.2008s.0.124.0

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  • The deformation rate and pattern of the Changhua Fault System, the middle western Taiwan(Poster session,Abstracts of the Taiwan and Japan Joint Symposium: "Geomorphological Hazards and Management" held on 17-18 March, 2008, at Taipei) :

    MATSUTA N., CHEN W, YU N., SHIH R., YANG C., CHU Y., ICHIN Y., HUANG N., YU Y., SU C

    29 ( 2 )   221 - 221   2008

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  • High-resolution P-wave seismic reflection imaging of the Kuwana active thrust: 2000 Inabe River profile

    Ishiyama Tatsuya, Matsuta Nobuhisa, Toda Shigeru, Sato Hiroshi, Kato Hajime, Takemura Keiji, Tsutsumi Hiroyuki, Okada Atsumasa, Ogisu Nobuhiro, Nakamura Kaneyuki, Takeuchi Syoko, Tani Miyuki, Ishii Sei, Nakanishi Toshimichi, Tajikara Masayoshi, Kimura Haruo, Hasegawa Shin, Sugito Nobuhiko, Kaneda Heitaro

    Bulletin of the Earthquake Research Institute,University of Tokyo   82 ( 1 )   75 - 84   2007

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    DOI： 10.15083/0000032488

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    Other Link： http://hdl.handle.net/2261/8152

  • High-resolution P-wave seismic reflection imaging of the Yoro active thrust: 2004 Shizu profile

    Ishiyama Tatsuya, Sato Hiroshi, Toda Shigeru, Nakanishi Toshimichi, Matsuta Nobuhisa, Sugito Nobuhiko, Tsutsumi Hiroyuki, Okada Atsumasa, Koike Taro, Imamura Tomohiro, Hattori Yasuhisa, Suzuki Norimasa, Amano Keigo, Kato Yoshito, Kawai Yohei, Takagi Keiji

    Bulletin of the Earthquake Research Institute,University of Tokyo   82 ( 1 )   65 - 74   2007

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    DOI： 10.15083/0000032487

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  • Reexamination of tectonic geomorphology of the southern part of the Matsumoto Basin and the southwestern margin of the Suwa Basin, along the middle part of the Itoigawa-Shizuoka Tectonic Line active fault system

    Sawa Hiroshi, Ando Toshihito, Kumamoto Takashi, Sano Shigeki, Nozawa Tatsujiro, Sakaue Hiroyuki, Watanabe Mitsuhisa, Suzuki Yasuhiro, Taniguchi Kaoru, Hirouchi Daisuke, Matsuta Nobuhisa, Uchida Chikara, Sato Yoshiki, Ishiguro Satoshi, Tajikara Masayoshi, Sugito Nobuhiko

    Active Fault Research   2007 ( 27 )   169 - 190   2007

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    We conducted a tectonic geomorphological survey in the southern part of the Matsumoto Basin and the south coast of the Suwa Basin, along the middle part of the Itoigawa-Shizuoka Tectonic Line (ISTL) active fault system. Procedures of this study are as follows; 1) aerial photo analysis and field surveys,2) mapping of geomorphic surfaces and reconstruction of geomorphic evolution,3) mapping of tectonic landforms which explain the geomorphic evolution reasonably,4) photogrammetrical measurement of vertical offset by construction of cross sections and calculation of vertical offset rates,5) measurement of horizontal offset of geomorphic markers and calculation of horizontal rates. Vertical/lateral offset rates were estimated based on vertical/lateral offset of geomorphic markers, such as terraces and ages of them (H: older than 120 ka, M1: 100 ka, M2: 40-65 ka, Lla: 20 ka, Lib: 10 ka, L2: 4-7 ka, L3: 1-2 ka). LiDAR method is also used for measurement of lateral offset<BR>Although mapped fault trace in the study area is similar to existing papers, different results were obtained in some areas. One of the remarkable results is that the Gofukuji fault in eastern margin of the Matsumoto Basin connects smoothly with the faults in northern end of the Suwa Basin. These faults have left lateral offset.<BR>We obtained 108 vertical/ left lateral offset rates in the study area. The vertical and leftlateral slip rates are estimated to be 0.1-2.0 mm/yr and 0.6-8.5 mm/yr, respectively.

    DOI： 10.11462/afr1985.2007.27_169

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  • Tectonic geomorphology of the northeastern margin of the Suwa Basin, along the middle part of the Itoigawa-Shizuoka Tectonic Line Active Fault System

    Tajikara Masayoshi, Uchida Chikara, Sakaue Hiroyuki, Kumamoto Takashi, Watanabe Mitsuhisa, Suzuki Yasuhiro, Sugito Nobuhiko, Sawa Hiroshi, Taniguchi Kaoru, Hirouchi Daisuke, Matsuta Nobuhisa, Sato Yoshiki, Ishiguro Satoshi, Ando Toshihito

    Active Fault Research   2007 ( 27 )   147 - 168   2007

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    We conducted a tectonic geomorphological survey in the northeastern margin of the Suwa Basin (in the area between Okaya and Chino), along the middle part of the Itoigawa-Shizuoka Tectonic Line Active Fault System (ISTL). Procedure of this study is as follows; 1) aerial photo analysis and field survey,2) mapping of geomorphic surfaces and reconstruction of geomorphic evolution,3) mapping of tectonic landforms which explains the geomorphic evolution reasonably,4) measurement of vertical offset by construction of cross sections and calculation of vertical offset rates,5) measurement of horizontal offset of geomorphic markers (e. g., terrace scarps, small valleys) and calculation of horizontal offset rates. Vertical/horizontal offset rates were estimated based on offset of geomorphic markers (fluvial terraces) and ages of the terraces (H, older than 120 ka; Ml,90-100 ka; M2,40-65 ka; Li a,20 ka; Lib,10 ka; L2,4-7 ka; L3,1-2 ka). Although mapped faults in this study are similar to existing papers, different results were obtained in some areas as follows; 1) we judged fault traces in existing papers near the Suwa Taisha Harumiya which lies on the right bank of the Togawa River is not a tectonic landform but an erosional scarp,2) we judged that broad gentle slope at Suwa Taisha Akimiya which is interpreted as flexural scarp is not a tectonic landform but a depositional landform of landslide deposits,3) we judged that the (fault) scarp in Kuwabara is not a tectonic landform but an erosional scarp,4) fault scarps which lie along boundary between the Suwa Basin and mountainous area at Uehara are newly mapped,5) the fault scarp near the Chino station at the right bank of the Kamikawa River is newly mapped as certainly located fault,6) the fault scarp which deforms L3 surface in a valley bottom at Sakamuro is newly mapped. We constructed 41 cross sections and obtained 47 vertical/lateral offset rates. Based on obtained vertical/horizontal offset rate, faults in the study area can be classified into three or four segments, although we could obtain only minimum vertical offset rates in many areas. The most southeastern segment is interpreted as a main fault which is inferred to construct a pull-apart basin. The other fault segments are interpreted as secondary faults of the main faults, based on the fact that these fault segments have short length (3-4 km), and that the fault segments have gentle round shaped fault traces.

    DOI： 10.11462/afr1985.2007.27_147

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  • Tectonic landform and excavation studies along and across the north-central part of the Itoigawa-Shizuoka tectonic line

    TANIGUCHI Kaoru, SUZUKI Yasuhiro, SAWA Hiroshi, MATSUTA Nobuhisa, WATANABE Mitsuhisa, Research Group for ISTL Tectonic Geomorphological

    Proceedings of the General Meeting of the Association of Japanese Geographers   2007 ( 71 )   78 - 78   2007

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    Language：Japanese   Publisher：The Association of Japanese Geographers  

    DOI： 10.14866/ajg.2007s.0.78.0

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  • Seismic reflection profiling across the central of the Itoigawa-Shizuoka tectonic line in Fujimi, central Japan

    Matsuta Nobuhisa, Ikeda Yasutaka, Sato Hiroshi, Imaizumi Toshifumi, Togo Masami, Kawamura Tomonori, Toda Shigeru, Miyauchi Takahiro, Kato Hajime, Echigo Tomoo, Tajikara Masayoshi, Ishiyama Tatsuya, Arai Yoshimasa, Ikawa Takeshi, Fujimi seismic profiling group

    Bulletin of the Earthquake Research Institute,University of Tokyo   82 ( 1 )   57 - 63   2007

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    Language：Japanese   Publisher：The University of Tokyo  

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  • Seismic reflection profiling across the northern part of the Itoigawa-Shizuoka tectonic line active fault system, Matsumoto, central Japan

    Matsuta Nobuhisa, Ikeda Yasutaka, Togo Masami, Imaizumi Toshifumi, Sato Hiroshi, Toda Shigeru, Tajikara Masayoshi, Kato Hajime, Ishiyama Tatsuya, Ikawa Takeshi, Matsumoto seismic profiling group

    Bulletin of the Earthquake Research Institute,University of Tokyo   82 ( 1 )   45 - 55   2007

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    DOI： 10.15083/0000032485

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    Other Link： http://hdl.handle.net/2261/8149

  • Seismic reflection profiling across the north of the Itoigawa-Shizuoka tectonic line in Omachi, central Japan

    Matsuta Nobuhisa, Ikeda Yasutaka, Sato Hiroshi, Imaizumi Toshifumi, Tajikara Masayoshi, Kurashimo Eiji, Kawamura Tomonori, Kato Naoko, Toda Shigeru, Tani Miyuki, Kato Hajime, Togo Masami, Nakamura Yousuke, Echigo Tomoo, Tanaka Atsuhiko, Ikawa Takeshi, Omachi seismic profiling group

    Bulletin of the Earthquake Research Institute,University of Tokyo   82 ( 1 )   37 - 44   2007

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    Language：Japanese   Publisher：The University of Tokyo  

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    DOI： 10.15083/0000032484

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    Other Link： http://hdl.handle.net/2261/8148

  • High-resolution seismic reflection survey "Oguro River seismic line" in the Ina Valley Fault Zone, central Japan: data acquisition and processing

    Okada Shinsuke, Ikeda Yasutaka, Oda Shin, Echigo Tomoo, Toda Shigeru, Suzuki Norimasa, Kawai Youhei, Kato Hajime, Sato Hiroshi, Kimura Haruo, Tajikara Masayoshi, Ishiyama Tatsuya, Imaizumi Toshifumi, Kagohara Kyoko, Matsuta Nobuhisa, Uchida Takuma, Uno Tomoki, Kawamura Tomonori

    Bulletin of the Earthquake Research Institute,University of Tokyo   82 ( 1 )   13 - 23   2007

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    DOI： 10.15083/0000032482

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  • P- and S-wave seismic reflection profiling across the Kamishiro fault, Itoigawa-Shizuoka Tectonic Line active fault system, central Japan

    Matsuta Nobuhisa, Ikeda Yasutaka, Sato Hiroshi, Imaizumi Toshifumi, Togo Masami, Yanagi Hiromi, Mikata Hitoshi, Toda Shigeru, Tsutsumi Hiroyuki, Kurashimo Eiji, Koshiya Shin, Noda Ken, Kato Hajime, Hirakawa Kazuomi, Yagi Kouji, Shishikura Masanori, Echigo Tomoo, Ishiyama Tatsuya, Haraguchi Tsuyoshi, Ogino Sumiko, Arai Yoshimasa, Kawamura Tomonori, Tajikara Masayoshi, Kato Naoko, Ikawa Takeshi, Kamishiro seismic profiling group

    Bulletin of the Earthquake Research Institute,University of Tokyo   82 ( 1 )   25 - 35   2007

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  • 糸魚川-静岡構造線活断層帯北部の白馬村・池田町におけるボーリング調査(速報)

    杉戸信彦, 澤祥, 田力正好, 松多信尚, 谷口薫, 鈴木康弘

    日本第四紀学会講演要旨集   37   2007

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  • 糸魚川-静岡構造線活断層帯中北部(松本~諏訪~茅野)の変動地形調査および航測解析による平均変位速度解明

    澤祥, 渡辺満久, 鈴木康弘, 谷口薫, 田力正好, 杉戸信彦, 廣内大助, 松多信尚, 鈴木康弘

    日本第四紀学会講演要旨集   37   2007

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  • Seismic reflection profiling across active folds in the eastern Shinjo basin, NE Japan

    佐藤比呂志, 八木浩司, 池田安隆, 今泉俊文, 荻野スミ子, 宮内崇裕, 戸田茂, 平野信一, 松多信尚, 越後智雄, 田力正好, 井川猛, 酒井隆太郎

    東京大学地震研究所彙報   81 ( 2 )   2007

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  • Active Tectonics of the Senya Hills and Evolution of the Senya Active Fault, Eastern Margin of the Yokote Basin Fault Zone, Northeast Japan

    KAGOHARA Kyoko, IMAIZUMI Toshifumi, MIYAUCHI Takahiro, SATO Hiroshi, UCHIDA Takuma, ECHIGO Tomoo, ISHIYAMA Tatsuya, MATSUTA Nobuhisa, OKADA Shinsuke, IKEDA Yasutaka, TODA Shigeru, KOSHIYA Shin, NODA Masaru, KATO Hajime, NODA Katsuya, MIWA Atsushi, KUROSAWA Hideki, KOSAKA Hideki, NOHARA Tsuyoshi

    Journal of Geography (Chigaku Zasshi)   115 ( 6 )   691 - 714   2006.12

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    The Eastern margin of the Yokote Basin Fault Zone (EYBFZ) is one of the seismogenic reverse faults that developed in Northeast Japan, generating the 1896 Rikuu Earthquake (M7.2). The EYBFZ is divided into range boundary fault (Kawaguchi Fault) and frontal fault. The major segment of the frontal fault consists of three faults : the Shiraiwa Fault, the Ota Fault, and the Senya Fault, at which coseismic surface ruptures with irregular and highly sinuous traces, gaps and echelon steps occurred during the 1896 Earthquake. In the study area, the irregular coseismic surface ruptures probably originate from differences in fault geometries and sedimentary conditions, which are associated with thrust-front migration in the Quaternary. We discuss the relationships among fault traces, geomorphic displacements, and fault geometries on the Senya Fault and the Kawaguchi Fault, based on data from high-resolution seismic reflection profiling, investigations into tectonic geomorphology and structural geology with the help of the balanced cross-section method.<BR>The seismic image obtained shows changes of geomorphic and geologic features around the Senya Hills expressed as differences in faulting geometries along the Senya Fault and the Kawaguchi Fault. In fact, the Senya Hills are situated as an unsymmetrical ordering.The disparity in the timing of thrust-front migration affects the development of fluvial surfaces, which are related to the appearance of the fault scarp on the surface. That is why, in the central portion of the Senya Hills, the Senya Fault is a typical emergent thrust with flat-ramp structures associated with the uplifting and the back-tilting of late Quaternary fluvial terraces. On the other hand, in the northern portion, the Senya Fault is a concealed thrust with step-like geometry and prominent folding and small faults in the hanging wall. The small faults infer the structure of the tectonic scarp and short wavelength deformation on the surface. This means that the Senya Fault at the central portion preceded the northern portion as an emergent fault. Moreover, fault traces show different dips between central and northern portions. The dip of the central portion is lower than that of the northern portion.<BR>By restoring the balanced cross-sections and assuming the uniform net-slip rate, the initial thrusting along the boundary faults is retroactive to 2.02.6 Ma at the central portion and 1.8 2.3 Ma at the northern portion. The initiation of thrust front migration from the boundary faults to the frontal faults is ca.1.6 Ma at the central portion and 0.6Ma at the northern portion.

    DOI： 10.5026/jgeography.115.6_691

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  • 17. Fault scarp waterfalls associated with 1999 Chi-Chi earthquake and their 6-year recession rates, western foothills in Taiwan(Abstracts of Papers Presented at the Fall Meeting of the Union, October 2005)

    HAYAKAWA Yuichi S., MATSUTA Nobuhisa, MATSUKURA Yukinori

    27 ( 1 )   107 - 107   2006

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  • 写真測量技術を導入した糸魚川-静岡構造線断層帯北部(栂池-木崎湖)の詳細変位地形・鉛直平均変位速度解析

    松多 信尚, 澤 祥, 安藤 俊人

    活断層研究   ( 26 )   105 - 120   2006

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  • High-resolution seismic reflection profiling across the Senya fault at Hanaoka, northern Honshu, Japan: Data acquisition and processing

    81 ( 2 )   97 - 106   2006

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  • High-resolution seismic reflection profiling across the Ota fault, eastern margin of the Yokote basin fault zone, northeast Japan: data acquisition and processing

    Kagohara Kyoko, Uchida Takuma, Miyauchi Takahiro, Imaizumi Toshifumi, Sato Hiroshi, Echigo Tomoo, Ikeda Yasutaka, Koshiya Shin, Noda Masaru, Matsuta Nobuhisa, Ishiyama Tatsuya, Toda Shigeru, Kato Hajime, Okada Shinsuke, Kato Naoko, Ogino Sumiko, Kimura Haruo, Watanabe Yuji, Uno Tomoki, Tanaka Tamaki, Kojima Jun, Ichikawa Fumihiro, Obata Kazuma, Norita Yasuyuki, Imamura Tomohiro, Noda Katsuya, Ikawa Takeshi

    Bulletin of the Earthquake Research Institute,University of Tokyo   81 ( 2 )   107 - 117   2006

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  • Study of tectonic landforms and late Quaternary slip rates along the northern part of the Itoigawa-Shizuoka tectonic line, between Omachi city and Matsumoto city.

    Sawa Hiroshi, Sakaue Hiroyuki, Kumamoto Takashi, Watanabe Mitsuhisa, Suzuki Yasuhiro, Tajikara Masayoshi, Taniguchi Kaoru, Hirouchi Daisuke, Matsuta Nobuhisa, Ando Toshihito, Sato Yoshiki, Ishiguro Satoshi, Uchida Chikara

    Active Fault Research   2006 ( 26 )   121 - 136   2006

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    We conducted a tectonic geomorphological survey along the northern part of the Itoigawa-Shizuoka Tectonic Line (ISTL) with support from the Ministry of Education, Culture, Sports, Science and Technology of Japan as one of the intensive survey on ISTL fault system. This survey aims to clarify the detailed distribution of the slip rates of this fault system, which provides the essential data set to predict the coseismic behavior and to estimate the strong ground motion simulation. In order to achieve this purpose, the active fault traces are newly mapped along the northern part of the ISTL through interpretations of aerial photographs archived in the 1940s and 1960s at scales of 1: 10,000 and 1: 20,000, respectively. This aerial photo analysis was also supplemented and reinforced by field observations.<BR>One of the remarkable results by using this data set is a large number of, here 84, photogrammetrically measured landform transections to quantify the tectonic deformations. We could calculate vertical slip rates of the faults at 74 points, based on the estimated ages of terraces (H: 120 kyrs, M: 50-100 kyrs, Ll: 10-20 kyrs, L2: 4-7 kyrs, L3: 1-2 kyrs). The vertical slip rates distributed in the northern part of the study area show 0.2-5.5 mm/yr on the L terraces (less than 20 kyrs) and 0.05-0.9 mm/yr on the M and H terraces (more than 50 kyrs). The vertical slip rates of the faults located in the central and southern part of the study area are 0.2-3.1 mm/yr.

    DOI： 10.11462/afr1985.2006.26_121

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  • High-resolution seismic reflection profiling across the Senya fault at the Unjono in the Yokote basin, northeast Japan : data acquisition and processing

    楮原京子, 今泉俊文, 佐藤比呂志, 宮内崇裕, 越後智雄, 松多信尚, 石山達也, 越谷信, 野田賢, 加藤一, 内田拓馬, 宇野知樹, 森泉俊行, 小田晋, 神田聡史, 森下信人, 水本匡起, 梅津洋輔, 小林勉, 氷高草多, 野田克也, 井川猛

    東京大学地震研究所彙報   81 ( 2 )   119 - 128   2006

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  • 糸魚川-静岡構造線活断層帯の地震時断層挙動および強震動の予測精度向上に資する変動地形調査

    鈴木康弘, 鈴木康弘, 渡辺満久, 渡辺満久, 澤祥, 澤祥, 廣内大助, 廣内大助, 隈元崇, 隈元崇, 松多信尚, 松多信尚, 田力正好, 田力正好, 谷口薫, 谷口薫, 佐藤善輝, 佐藤善輝, 石黒聡士, 石黒聡士, 安藤俊人, 安藤俊人, 内田主税, 内田主税, 佐野滋樹, 佐野滋樹, 野澤竜二郎, 野澤竜二郎, 坂上寛之, 坂上寛之

    日本第四紀学会講演要旨集   ( 36 )   2006

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  • 横手盆地東縁断層帯の活構造

    楮原京子, 今泉俊文, 越智智雄, 宮内崇裕, 越谷信, 野田賢, 戸田茂, 加藤一, 佐藤比只志, 荻野スミ子, 池田安隆, 松多信尚, 石山達也, 三輪敦志, 黒澤英樹, 野田克也, 井川猛

    日本第四紀学会講演要旨集   ( 36 )   2006

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  • 伊那谷断層帯の構造とその発達過程

    岡田真介, 池田安隆, 小田晋, 越後智雄, 戸田茂, 鈴木規眞, 天野桂悟, 加藤一, 佐藤比呂志, 木村治夫, 田力正好, 石山達也, 今泉俊文, 楮原京子, 松多信尚, 内田拓馬

    日本第四紀学会講演要旨集   ( 36 )   2006

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  • 台湾中部の衝突帯前縁部,后里台地・大肚山丘陵地域の活断層と上部地殻の変形様式

    松多信尚, CHEN Wen-Shan, YANG Chi-Cheng, YAN Yi-Iching, SHIH Ruey-Chyuan, SUNG Shih-Hwa, HUANG Neng-Wei

    日本第四紀学会講演要旨集   ( 36 )   2006

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  • Shallow seismic reflection survey across the North Matsuda fault in the Kozu-Matsuda fault system, central Japan

    Kimura Haruo, Ogino Sumiko, Kagohara Kyoko, Oda Shin, Node Katsuya, Ikawa Takeshi, Sato Hiroshi, Ito Tanio, Miyauchi Takahiro, Matsuta Nobuhisa, Kawamura Tomonori, Ishiyama Tatsuya, Okada Shinsuke, Kato Naoko

    Active Fault Research   2005 ( 25 )   85 - 92   2005

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    The North Matsuda fault in the Kozu-Matsuda fault zone is one of the active fault system, showing the largest vertical component of slip rate onshore Japanese islands. The Kozu-Matsuda fault system is considered as a part of the northern margin of the Philippine Sea plate. It is necessary to obtain the horizontal shortening component of slip rate of the North Matsuda fault for a better understanding of active tectonics in the northern margin of the Philippine Sea plate. To reveal the subsurface structure of the North Matsuda fault, high-resolution shallow seismic reflection survey with about 3.2 km line length was carried out across the fault, A kind of accelerated weight drop system named as Yuatsu Impactor (JGI Inc. ) was used as seismic source which has wide band frequency spectrum. Both the standard shot intervals and group intervals of geophones were 10 m. The Sakawa River near the center of the line obstructed both shooting and geophone setting, and the half of the line in the Matsudayama Mountains was severely crooked. Although such a bad survey conditions, the seismic section after careful data processing shows a drastic structural change and a north dipping thrust fault with 18 degrees near the Sakawa River, which is suggested as the North Matsuda fault. The fault trace revealed by a result of the seismic reflection survey is exactly located along the Sakawa River.

    DOI： 10.11462/afr1985.2005.25_85

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  • 糸魚川-静岡構造線活断層系北部は危険が切迫している活断層なのか? (総特集 陸域震源断層--深部すべり過程のモデル化) -- (3章 糸魚川-静岡構造線の調査)

    松多 信尚

    号外地球   ( 50 )   191 - 196   2005

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  • 糸魚川-静岡構造線活断層系北部の活動に関連した犀川丘陵の変動地形

    田力 正好, 松多 信尚

    活断層研究   ( 25 )   63 - 73   2005

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  • 伊那谷断層帯北部における反射法地震探査

    小田晋, 池田安隆, 越後智雄, 岡田真介, 戸田茂, 鈴木規真, 河合陽平, 天野桂悟, 高木啓司, 加藤義人, 石山達也, 今泉俊文, かご原京子, 加藤一, 松多信尚, 田力正好, 内田拓馬, 宇野智樹, 佐藤良

    日本地震学会秋季大会講演予稿集   2005   2005

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  • 陸域震源断層深部すべり過程のモデル化 反射法地震探査による北部フォッサマグナの地殻構造

    佐藤比呂志, 岩崎貴哉, 川崎慎治, 池田安隆, 松多信尚, 加藤直子, 武田哲也, 川中卓, 井川猛

    月刊地球   2005

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  • 陸域震源断層深部すべり過程のモデル化 北部フォッサマグナ周辺の屈折法探査データの再解析による地殻構造の解明

    武田哲也, 佐藤比呂志, 岩崎貴哉, 松多信尚, 酒井慎一, 飯高隆, 加藤愛太郎

    月刊地球   2005

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  • 陸域震源断層深部すべり過程のモデル化 糸魚川-静岡構造線活断層系北部は危険が切迫している活断層なのか?

    松多信尚

    月刊地球   2005

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  • O-150 Structure of Matsuda-Kita fault in Kozu-Matsuda fault zone revealed by seismic reflection survey

    Kimura H, Ogino S, Kagohara K, Oda S, Ishiguro A, Hasegawa S, Kamijo H, Komada N, Maruyama T, Sakashita N, Mori T, Sato H, Sano J, Noda K, Ikawa T, Ito T, Miyauchi T, Matsuta N, Kawamura T, Ishiyama T, Okada S, Kato N

    Annual Meeting of the Geological Society of Japan   2004   100 - 100   2004

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    Language：Japanese   Publisher：The Geological Society of Japan  

    DOI： 10.14863/geosocabst.2004.abst.0_100_2

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  • 糸魚川-静岡構造線活断層系の断層活動と犀川丘陵の変動地形

    松多信尚, 田力正好

    日本地震学会秋季大会講演予稿集   2004   2004

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  • 北部フォッサマグナ,犀川丘陵内における糸魚川-静岡構造線活断層系の活動に関連した地殻変動

    田力正好, 松多信尚

    日本第四紀学会講演要旨集   ( 34 )   2004

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  • Partitioning of slip on the ltoigawa-Shizuoka Tectonic Line active fault system ,central Japan,in Quaternary time

    MATSUTA Nobuhisa, IKEDA Yasutaka

    63 ( 63 )   112 - 112   2003.3

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  • Structure and behavior of the Tectonic Line active fault system, central Japan, in Quaternary time

    MATSUTA Nobuhisa, IKEDA Yasutaka

    63 ( 63 )   237 - 237   2003.3

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  • 糸魚川-静岡構造線活断層系北部の平均すべり速度

    松多信尚, 田力正好, 河村知徳, 池田安隆

    日本地震学会秋季大会講演予稿集   2003   2003

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  • Structure and behavior of the Itoigawa-Shizuoka Tectonic Line, Central Japan, in Quaternary Time : partitioning of slip on an oblique-slip fault zone

    MATSUTA N.

    Abstract, IUGG, 2003   2003

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  • High-Resolution Seismic Reflection Profile across at the Western Flank of the Umaoi Hills, the Frontal Part of Hidaka Thrust System, Hokkaido

    Kato Naoko, Sato Hiroshi, Matsuta Nobuhisa

    Bulletin of the Earthquake Research Institute,University of Tokyo   77 ( 2 )   111 - 121   2002

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  • Structure and Behavior of the Itoigawa-Shizuoka Tectonic Line, Central Japan, in Quaternary Time : Partitioning of Slip on an Oblique-Slip Fault Zone

    MATSUTA N.

    PhD Thesis, Univ. Tokyo   2002

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  • 糸魚川-静岡構造線活断層系北部神城断層の浅部構造と平均すべり速度(浅部反射法地震探査とボーリングの結果)

    松多 信尚, 池田 安隆, 今泉 俊文

    活断層研究   ( 20 )   59 - 70   2001

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  • High resolution, very shallow seismic reflection profiling across active faults: a case study of the Senya fault, Akita Prefecture, Northeast Japan

    Matsuta Nobuhisa, Abe Shinro, Imaizumi Toshifumi, Pratt Thomas, Williams Robert, Sato Hiroshi, Kurashimo Eiji, Kato Naoko, Ogino Sumiko, Moriya Hiroshi

    Active Fault Research   2001 ( 20 )   40 - 45   2001

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    A high-resolution P-wave seismic reflection profile was acquired across the toe of the Senya thrust, northern Honshu, Japan, to test the applicability of profiling using a hummer source (3.5 kg). Seismic data was recorded by a portable recording system (60 ch), with 28Hz geophones spaced at 0.5m intervals, and processed by standard Common Mid-Point (CMP) method. The obtained seismic section clearly demonstrates an eastdipping thrust down to 40-m in depth. The geometry of the thrust well fit to the subsurface structure estimated by drill core data.

    DOI： 10.11462/afr1985.2001.20_40

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  • 2-D and 3-D Subsurface Density Structure in the Northern Part of the Itoigawa-Shizuoka Tectonic Line Derived by Gravity Surveying

    OKUBO Shuhei, IKEDA Yasutaka, KUMAMOTO Takashi, SETA Gaku, MATSUTA Nobuhisa, CHIBA Hiroaki, ARAI Yoshimasa

    Journal of the Geodetic Society of Japan   46 ( 3 )   177 - 186   2000.9

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    We carried out gravity surveying along a profile of the reflection seismological prospecting in the northern part of the Itoigawa-Shizuoka Tectonic Line (ISTL). Combined use of gravity and seismic data enables us to construct a 2-D subsurface density model. We also pre sent a 3-D model which is consistent with the previous works on gravity and reflection/refraction prospecting. Both 2-D and 3-D models show a reverse fault structure dipping toward the east. We do not find any thrusting structure dipping toward the west as implied from the up lifting of the Hida range.

    DOI： 10.11366/sokuchi1954.46.177

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  • 糸魚川静岡構造線活断層系中部-富士見地域-における断層の地下形状とスリップパーティショニング

    松多信尚, 今泉俊文, 東郷正美, 佐藤比呂志, 沢祥, 石山達也, 越後智雄, 中村洋介, 田中靖之

    日本地震学会秋季大会講演予稿集   2000   2000

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  • 極浅層反射法探査による活断層のイメージング 千屋断層・富士見断層群を例として

    松多信尚, 今泉俊文, PRATT T, WILLIAMS R, 佐藤比呂志, 池田安隆, 蔵下英司, 荻野スミ子, 加藤一

    日本地震学会秋季大会講演予稿集   2000   2000

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  • 石狩低地東縁断層帯・馬追丘陵を横切る反射法地震探査(中間報告)

    加藤直子, 松多信尚, 平川一臣, 越谷信, 宮内崇祐, 戸田茂, 加藤一, 川中卓, 井川猛

    日本地震学会秋季大会講演予稿集   2000   2000

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  • Estimated subsurface Itoigawa-Shizuoka Tectonic Line along the Southeastern Rim of Matsumoto Basin and evolution of Fukashi Basin,central Japan

    MATUTA Nobuhisa, IKEDA Yasutaka

    56 ( 56 )   82 - 83   1999.10

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  • Tectonics along the southeastern rim of Matsumoto basin considered from seismic profiling and tectonic landform

    MATSUTA N.

    Master thesis, Graduate School of Science, Univ. of Tokyo   1999

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  • Strike-slip rate of the southern part of Gofukuji fault, Itoigawa-Shizuoka Tectonic Line, central Japan.

    松多信尚, 池田安隆

    地球惑星科学関連学会合同大会予稿集   1998   1998

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  • Precise mapping of active faults along the Itoigawa-Shizuoka Tectonic Line in the southern part of Matsumoto Basin.

    池田安隆, 松多信尚, 東郷正美, 今泉俊文, 佐藤比呂志

    活断層研究   ( 16 )   28 - 34   1997.8

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  • 神戸周辺地域の活断層の活動度

    渡辺 満久, 鈴木 康弘, 広内 大助, 尾崎 陽子, 奥野 慎太郎, 松多 信尚, 加藤 雅彦

    日本地理学会予稿集   49   182 - 183   1996.3

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  • 飛騨山脈東部の活断層「烏川断層」の発見と変位速度の推定

    小口 高, 青木 賢人, 松多 信尚

    日本地理学会予稿集   49   186 - 187   1996.3

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  • On the latest paleoseismic event of the Tachikawa fault in the Tokyo metropolitan area

    TOGO Masami, SATO Hiroshi, IKEDA Yasutaka, MATSUTA Nobuhisa, MASUBUCHI Kazuo, TAKANO Shigeaki

    Active Fault Research   1996 ( 15 )   1 - 8   1996

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    Language：Japanese   Publisher：Japanese Society for Active Fault Studies  

    By excavation of the Ochikawa-Ichinomiya remain located on the flood plain along Tama River near the boundary between Tama City and Hino City, Tokyo metropolitan area, a fault was found in young alluvium. This fault is regarded as the continuation of Tachikawa fault, a major active fault existing in the left bank area of Tama River, because it is located on the southeastern extension of Tachikawa fault line, and its strike is almost parallel to the Tachikawa fault.<BR>Detailed investigation of the fault outcrop made it clear that the last faulting event on the Tachikawa fault had occurred after A. D.1020-1158, the mid-Heian period. At this place, the last faulting event was dominantly strike slip with horizontal shortening of about 0.6 m.

    DOI： 10.11462/afr1985.1996.15_1

    CiNii Article

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  • Latest paleoseismic event of Tachikawa fault.

    東郷正美, 佐藤比呂志, 池田安隆, 松多信尚, 増淵和夫, 高野繁昭

    日本地震学会秋季大会講演予稿集   1996   1996

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Awards

  • 論文業績賞（奨励賞）

    2020.6   物理探査学会   横ずれ断層における各種物理探査の適用可能性の検討（その1：浅層反射法地震探査・屈折法地震探査・CSAMT 探査・重力探査）―郷村断層帯および山田断層帯における事例―

    岡田真介・坂下 晋・今泉俊文・岡田篤正・中村教博・福地龍郎・松多信尚・楮原京子・戸田 茂・山口 覚・松原由和・山本正人・外處 仁・今井幹浩・城森 明

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  • 日本地理学会賞（著作発信部門）

    2020   日本地理学会   救援物資輸送の地理学：被災地へのルートを確保せよ

    荒木一視・岩間信之・楮原京子・熊谷美香・田中耕市・中村努・松多信尚

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  • 物理探査学会奨励賞

    2020   物理探査学会   横ずれ断層における各種物理探査の適用可能性の検討（その1：浅層反射法地震探査・屈折法地震探査・CSAMT 探査・重力探査）―郷村断層帯および山田断層帯における事例―

    岡田真介・坂下 晋・今泉俊文・岡田篤正・中村教博・福地龍郎・松多信尚・楮原京子・戸田 茂・山口 覚・松原由和・山本正人・外處 仁・今井幹浩・城森 明

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    Award type：Honored in official journal of a scientific society, scientific journal  Country：Japan

  • 学会賞

    2017   地域地理科学会  

    松多信尚

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  • 日本地理学会賞（著作発信部門）

    2016   日本地理学会  

    鈴木康弘 会員ほか執筆者一同

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  • 学会賞（社会貢献部門）

    2012   日本地理学会  

    鈴木康弘, 松多信尚ほか, 日本地理学会災害対応本部津波被災マップ作成チーム

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  • 論文賞

    2011   日本活断層学会   平均変位速度分布に基づく糸魚川－静岡構造線断層帯北部の地震発生予測

    鈴木 康弘 杉戸 信彦 隈元 崇 澤 祥 渡辺 満久 松多 信尚 廣内 大助 谷口 薫 田力 正好 石黒 聡士 佐藤 善輝 活断層研究

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Research Projects

  • Development of Integrated Geomorphological Interpretation Support System Based on the Wisdom of Geomorphologists - Utilization of eye-tracking and AI

    Grant number：24K00174  2024.04 - 2027.03

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research  Grant-in-Aid for Scientific Research (B)

    佐藤 剛, 松多 信尚, 奈良間 千之, 史 中超, 八木 浩司

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    Grant amount：\18070000 （ Direct expense: \13900000 、 Indirect expense：\4170000 ）

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  • 2023年5月5日の地震を含む能登半島北東部陸海域で継続する地震と災害の総合調査

    Grant number：23K17482  2023.06 - 2024.03

    日本学術振興会  科学研究費助成事業  特別研究促進費

    平松 良浩, 岡田 知己, 吉田 圭佑, 高木 涼太, 篠原 雅尚, 酒井 慎一, 藏下 英司, 西村 卓也, 太田 雄策, 木下 陽平, 宮崎 真一, 後藤 忠徳, 笠谷 貴史, 吉村 令慧, 田中 愛幸, 宮澤 理稔, 荒木 英一郎, 森下 知晃, 鹿児島 渉悟, 石山 達也, 立石 良, 安江 健一, 廣内 大助, 松多 信尚, 宍倉 正展, 岩田 知孝, 浅野 公之, 大堀 道広, 村田 晶, 石川 浩一郎, 山岸 邦彰, 須田 達, 山崎 新太郎, 青木 賢人, 林 紀代美, 武田 公子, 田中 純一, 井口 克郎, 佐々木 大輔, 原 裕太, 吉田 浩

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    Grant amount：\29640000 （ Direct expense: \22800000 、 Indirect expense：\6840000 ）

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  • An integrated understanding of tectonics based on mechanical properties exploration of the island-arc crust

    Grant number：23H01270  2023.04 - 2028.03

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research  Grant-in-Aid for Scientific Research (B)

    鷺谷 威, 寺川 寿子, 松多 信尚, MenesesーGutierrez Angela

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    Grant amount：\18330000 （ Direct expense: \14100000 、 Indirect expense：\4230000 ）

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  • Temporal changes of Quaternary crustal uplift rates of Japanese islands revealed by terrestrial in-situ cosmogenic nuclide daying

    Grant number：23H00723  2023.04 - 2027.03

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research  Grant-in-Aid for Scientific Research (B)

    石山 達也, 安江 健一, 若狭 幸, 松多 信尚, 廣内 大助

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    Grant amount：\18590000 （ Direct expense: \14300000 、 Indirect expense：\4290000 ）

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  • 土石流危険渓流の安全度評価手法の確立 ―重力探査による谷中に堆積する土砂の見 積もりと土石流発生ポテンシャル評価―

    2022.07 - 2023.03

    公益財団法人 八雲環境科学振興財団  環境研究助成申請書 

    松多信尚 住田達哉, 楮原京子 石黒聡士

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    Authorship：Principal investigator 

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  • 三瓶火山の最新活動と噴火形態

    2022.07 - 2023.03

    ウェスコ学術振興財団  令和4年度学術研究費助成事業【研究費助成】助成 特定研究分野A 

    松多信尚 楮原京子

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    Authorship：Principal investigator 

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  • 能登半島北東部において継続する地震活動に関する総合調査

    Grant number：22K19949  2022.07 - 2023.03

    日本学術振興会  科学研究費助成事業  特別研究促進費

    平松 良浩, 藏下 英司, 酒井 慎一, 飯高 隆, 勝間田 明男, 岡田 知己, 吉田 圭佑, 西村 卓也, 太田 雄策, 木下 陽平, 吉村 令慧, 後藤 忠徳, 笠谷 貴史, 田中 愛幸, 宮澤 理稔, 森下 知晃, 鹿児島 渉悟, 石山 達也, 安江 健一, 廣内 大助, 松多 信尚, 大堀 道広, 村田 晶, 岩田 知孝

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    Grant amount：\39780000 （ Direct expense: \30600000 、 Indirect expense：\9180000 ）

    能登半島北東部で長期間継続する地震活動の原因及び全体像、また2022年6月19日のマグニチュード5.4、最大震度６弱の地震による災害像を明らかにするために、地震観測、測地観測、電磁気観測、重力観測、温泉成分測定、活構造調査、強震観測からなる総合調査を2022年7月から2023年3月まで実施した。
    これらの観測で得られたデータの解析により、複数の断層面で地震が発生していることや震源が時空間的に移動していること、震源域南部の深部に流体の存在を示す地震波速度構造や比抵抗構造が存在すること、地震波の反射波から推定される反射面も深部の流体の存在と整合的であること、地殻変動源の位置が時間的に変化するとともに地殻変動源のモデルが開口割れ目から開口を伴う逆断層に変化したこと、震源域北部において重力値が減少し、地殻変動源のモデルと概ね一致すること、温泉成分の陰イオン濃度が複数地点で同時期に時間変化をし、地殻流体の影響を反映した可能性が考えられること、年代指標となる火山灰に基づき海成段丘面の年代を特定し、その分布高度と合わせて隆起速度を推定したこと、地震活動域の東部から南部にかけての海成段丘面で新たな変動地形を見出したこと、震度６弱の記録地点周辺において、工学的基盤面での速度コントラストの大きさが地震動増幅に大きく寄与していることや卓越周波数の空間変化があること、を研究成果として得ることができた。
    これらの成果は非火山地域における群発地震活動の要因を考える上で重要なものであり、また当該地域における地震防災に役立つ知見も得られており、科学的・社会的にも意義がある成果である。

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  • Disaster prevention education by increasing understanding of local characteristics and its effectiveness verification

    Grant number：22K18507  2022.06 - 2025.03

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research  Grant-in-Aid for Challenging Research (Exploratory)

    松多 信尚, 岡崎 善弘, 廣内 大助, 内山 琴絵

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    Grant amount：\6240000 （ Direct expense: \4800000 、 Indirect expense：\1440000 ）

    本研究の目的は「地域を見る見方・考え方」を習得することで、その後の生活の中で地域認知度を上げ防災力向上につなげる体験的な地域学習を試み、その効果を実証することである。本年度は、岡山市富山中学校で、防災教育と地域教育とを結びつける教材開発を施行し、地域に即した防災ゲームを作成し、公民館で地域の住人に対してイベントをすることで、地域住民に対する防災に資する地域認知活動を模索した。
    岡山市中区富山地区は岡山市街地からバスで２０分程度のところに位置し、東を一級河川旭川の旧河道を利用した放水路である百間川が流れ、北側を花崗岩質の丘である操山、南を江戸時代に干拓された０ｍ地帯が分布している。開発は高度経済成長期より急速に進んだ地域である。まず1学期に３年生が課外活動に合わせた事前活動で災害について学び、防災に関する問題を配置した防災双六を作り、学年全員がそのすごろくを授業で遊ぶことで、災害について知識を共有した。次に課外活動で淡路島の北淡地震記念館に行き、災害について学習し、自分たちが作った双六のブラッシュアップを考えた。２学期に２年生の生徒会に所属する生徒が引き継ぎ、放課後、ファシリテータとして修士の大学院生と学部生が参加し５回にわたり１－１時間半程度の活動を行った。その際、平成３０年西日本豪雨の後で倉敷市真備町の岡田地区で作成された発災時や災害後の行動を記録し伝える「にげる」「いきる」という二冊の冊子をもとに、災害を発災前から災害後までの時間軸でとらえることや、地域の特性に合わせた地理的空間の把握の重要性を理解させ、効果的に必要なことを学べる防災ゲームを作成した。
    それを地区の公民館で地域住民に実施し、地域貢献として、地域の住民の防災知識の向上に役立てた。
    このほか、自然現象の言葉を理解の確度調査を行い、その効果的な学習方法を模索する実験の準備が整った。

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  • Relationship between Strain Accumulation Processes and Surface Rupture along the Longitudinal Valley Fault, Taiwan

    Grant number：22H00754  2022.04 - 2025.03

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research  Grant-in-Aid for Scientific Research (B)

    松多 信尚, 松岡 格, 廣内 大助, 杉戸 信彦, 早川 裕弌, 石山 達也, 村瀬 雅之

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    Grant amount：\17160000 （ Direct expense: \13200000 、 Indirect expense：\3960000 ）

    本年度の9月に当該地域に地震が発生し、本研究が対象とする台東縦谷断層沿いに地表地震断層が出現した。この地震は本研究が想定していた海岸山脈を隆起させる東傾斜の逆断層ではなく、中央山脈が上がる西傾斜の断層による地震であった。そこで、本年は地表地震断層の位置を確認し、変位があった地点を横切る水準測量の測線で上下変位量を測量した。また、地表地震断層が出現した地域を中心に当該地域の活断層を空中写真判読から判読した。
    その結果、東竹地区では、従来観測されていたクリープ運動の変位とは逆の西上がりの変位がクリープ断層と同じ地点で見られた。また、変位パターンも西上がりの変位が見られた。玉里地区では従来のクリープ地点では大きな変位が認められず、別の場所で西上がりの変位が見られ、瑞穂地域では明瞭な地表変位は認められないが、水準測量では西上がりの変位が見られ、これは地形で認められる活断層と一致することがわかった。
    同地域の活断層調査では、従来報告されている活断層トレースとは別にいくつか活断層のトレースが認められ、地形発達を考えるうえで、長期間の変位速度や活動履歴を確認できる調査候補地を複数見つけることができた。また、地表地震断層が出現した場所では明瞭な活断層が認められない地点も多いが、段丘面の形状などで事前に推定できた可能性もわかった。中央山脈側の西傾斜の断層は明瞭なものはないが、数か所で変動地形としか考えられない地点を見つけられた。
    地表地震断層が出現した地点の日本統治時代の地籍図調査は収集を始めているが、まだ十分な議論ができていない。

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  • 断層活動の不均一性を考慮した大規模活断層帯の地震予測モデルの構築

    Grant number：22H00752  2022.04 - 2025.03

    日本学術振興会  科学研究費助成事業  基盤研究(B)

    廣内 大助, 竹下 欣宏, 安江 健一, 松多 信尚, 杉戸 信彦, 石山 達也

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    Grant amount：\17420000 （ Direct expense: \13400000 、 Indirect expense：\4020000 ）

    本研究では断層帯の一部が活動した地震の特性を明らかにし、糸静線など大規模活断層帯における地震規模やセグメンテーションなどの仕組みを解明し，地震予測モデルの構築をめざしている．初年度である2022年度には、糸魚川ー静岡構造線活断層帯北部をターゲットとし、2014年神城断層地震で活動しなかった神城断層帯南半分における過去の詳細な活動履歴を調べるべく、トレンチ掘削調査を実施した。また断層帯の地形地質調査も実施した。掘削調査は白馬村の南神城地点である。断層で東側が隆起した丘陵と低地の境界付近を掘削したところ、約3m堆積した黒色腐植土層が出現した。腐植土層は断層によって西側へ傾斜する傾斜不整合の構造を示しており、また一部は副次的な断層によって切断されている。これら傾斜不整合と副次断層の切断と地層の被覆関係から、少なくとも過去３回の断層活動を読み取ることができた。地層はこれまでの年代測定結果に基づくと、今回の試料から、掘削溝の下部で約3750年前であり、それ以降に約3回の活動があった可能性を示唆する。今後詳細な層相解析と追加年代測定を実施し、本地点における詳細な活動履歴を明らかにする予定である。

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  • 外的条件の変化による活断層の活動性への影響

    Grant number：19K21665  2019.06 - 2024.03

    日本学術振興会  科学研究費助成事業  挑戦的研究(萌芽)

    松多 信尚, 廣内 大助, 杉戸 信彦, 佐藤 善輝, 石山 達也

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    Grant amount：\6240000 （ Direct expense: \4800000 、 Indirect expense：\1440000 ）

    本研究の遂行には、年稿がある場所であること、地震のイベントが読めることが、必須条件である。2019年度は既存の調査結果の詳細な検討や、予察的な調査を行い、調査地点、および調査手法の検討を行った。その結果、調査地点は4か所を検討し、3か所に絞られた。第一地点は奥村ほか(1998）、今泉ほか(1996）の調査地点である。この地点は松多ほか(2001）によるボーリング調査ですでに年稿が確認できており、その後丹羽ほか(2018）など年代結果が多数あることから、それらも参考にできることが利点である。ただ、この地点は支流性の礫層が多く挟まれるため、年稿が連続的にならない課題がある。第二地点は下川ほか（1987）の調査地点である。この地点の報告は学会の予稿集しかなかったため、著者等と連絡を取り当時の資料を開示していただいた。その結果、この地点でも年稿と思われる記載がみられ候補地として有力なことが分かった。ただ湖の深度が深い可能性があり、地震イベントを読み取れない可能性があることが課題である。第三の地点は盆地中央部である。この地点は掘削地点が適当であれば湖の湖畔に位置し地震による環境変化が大きいと思われる。特に湖畔の泥炭層が発達している場合など、年代試料も豊富に得られる可能性がある。ただ年稿の形成が酸素不足による生物の不活発であるとすれば、湖の深度が浅いために年稿がない可能性がある。近辺で調査をした産総研の近藤さんの掘削結果を聞けばその可能性が高いことが確認された。第四地点はクロスカントリー会場へとつながる谷の出口である。この地点は当初最有力地点であったが、産総研の調査結果をうかがうと、礫層がみられることと、断層が低角になっており、断層の位置を特定しにくいことが判明し、候補地から除外した。

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  • 断層活動の多様性を考慮した活断層地震予測モデルの再構築

    Grant number：19H01373  2019.04 - 2022.03

    日本学術振興会  科学研究費助成事業 基盤研究(B)  基盤研究(B)

    廣内 大助, 竹下 欣宏, 安江 健一, 松多 信尚, 杉戸 信彦, 藤田 奈津子, 石山 達也

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    Grant amount：\17420000 （ Direct expense: \13400000 、 Indirect expense：\4020000 ）

    2014年神城断層地震や2016年熊本地震は、国が想定で用いているいわゆる固有の最大規模地震ではない地震であった。これらの地震が断層帯全体の繰り返し間隔など活断層の活動特性とどのように関わるのかについて明らかにし、内陸直下型地震の長期予測評価手法の改善を目指すことを目的としている。
    2019年には2014年にM6.7の一回り小さな地震を発生させた神城断層において、過去の活動履歴を明らかにするためのトレンチ掘削調査を実施した。トレンチでは明瞭な断層と地層の変形が認められ、2014年の活動を含め、少なくとも３回の地震活動の痕跡を見出すことができた。一つ前の地震はおよそ340±30yrBP以降、2014年以前、二つ前の活動は、1710±30yrBP以降、340±30yrBp以前となる。
    これに対応する歴史地震は一つ前の活動が1714年の小谷地震、二つ前の活動が762年の美濃・飛騨・信濃の地震もしくは、841年信濃の地震の可能性が高く、精度の高い古地震活動データを得ることができた。
    また次年度に向けて、2014年地震同様に一回り小さな地震であった、2000年中越地震の起震断層となった小平尾断層、六日町盆地西縁断層帯の概査を実施し、次年度以降の調査地点の目星をつけることができた。また2000年に活動していない、六日町盆地西縁断層帯南部においても、新たな変動地形を多数確認した。これらについても、地形形成年代と変位量、可能であればトレンチ掘削調査を次年度以降検討していく。

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  • Diversity of Nankai Trough earthquakes revealed by Holocene geomorphic development

    Grant number：18H00765  2018.04 - 2022.03

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (B)  Grant-in-Aid for Scientific Research (B)

    MATTA NOBUHISA

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    Grant amount：\17290000 （ Direct expense: \13300000 、 Indirect expense：\3990000 ）

    The purpose of this study was to explicitly show the diversity of Nankai Trough earthquakes and the existence of low-frequency super earthquakes by focusing on beach ridges and sand dunes. Specifically, we reexamined the developmental history of the Kikukawa Lowland, estimated uplift rates, and attempted to clarify formation process of the beach ridge sequence. As a method, we attempted to estimate the basement and Holocene marine sediments depth by making full use of geophysical surveys such as tight-lattice gravity survey, shallow reflection seismic survey, microtremor survey, and GPR survey.
    These surveys revealed that buried terraces and incised-valleys that cut the terraces were found under the Kikugawa Lowland, and the landform evolution since the middle Holocene has been influenced by the paleo-topography. The uplift rate was estimated to be approximately 1-1.6 mm/yr.

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  • Interaction between plate subduction and long inland strike-slip fault: Sumatran fault after the occurrence of a giant earthquake

    Grant number：17H04577  2017.04 - 2020.03

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (B)  Grant-in-Aid for Scientific Research (B)

    TABEI Takao

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    Grant amount：\16250000 （ Direct expense: \12500000 、 Indirect expense：\3750000 ）

    Sumatran fault in Sumatra island, Indonesia is the long inland strike-slip fault running parallel to the plate subduction boundary at the Sunda Trench. Reactivation of fault movement has been expected along the Sumatran fault because the 2004 Sumatra-Andaman giant earthquake caused regional stress increase on its fault plane. In this study we conducted dense GNSS observation, microtremor exploration and geomorphic field survey along two branch segments of the Sumatran fault near urban areas in Aceh Province, Sumatra. We estimate current locking/slip distribution on the fault plane and subsurface structure of the fault together with long-term fault slip history. These results will provide fundamental data for estimating earthquake generation potential in the near future.

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  • 浅層反射法地震探査を用いた2014年神城断層地震時のネットでの変位量分布

    Grant number：17H05315  2017.04 - 2019.03

    日本学術振興会  科学研究費助成事業 新学術領域研究(研究領域提案型)  新学術領域研究(研究領域提案型)

    松多 信尚

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    Grant amount：\2860000 （ Direct expense: \2200000 、 Indirect expense：\660000 ）

    上部地殻で発生する地震を評価するためには，過去の地震の痕跡である活断層から推定することが有効であるため，地表における地震の痕跡と実際の地震との関連性を明らかにする必要があり，地表地震断層が出現した地震は数少ない機会となる．そこで，本研究は地表地震断層の地表での変位が調べられている2014年11月22日に長野県北部白馬村を震源とした地震（Mw 6.2）に伴い出現した地表地震断層の地下数10 mにおける断層の形状および地質構造を高解像度でイメージングすることを目的とした極浅層S波反射法地震探査を実施した．本探査は，2017年11月および2018年11月に長野県白馬村内の地表地震断層を横切る6測線（塩島測線・大出北測線・大出南測線・ウイング21測線・飯森測線・堀之内測線）において実施した．震源にはGEOSYM社製の可搬型S波スィープ震源ELVISを用いた．スイープ周波数は20～120 Hz，スィープ長は10秒である．受振には96チャンネルのSHジオフォンを装備したランドストリーマー（固有周波数14 Hz）を使用した．発震点間隔は1 m（ウイング21測線のみ発震点間隔2 m），受振点間隔は50 cmとした．また，探鉱器にはGeoMetrix社製のGEODEを使用し，サンプリング間隔を1 msecとして観測を行った．
    一般的な共通反射点重合法による解析の暫定的な結果では、地表近傍から最大で深度100 mまでの断層の規模・形状および地質構造をイメージングすることができた．明らかになった断層の位置と形状から，ネット量での変位量の分布は地表地震断層調査結果とは異なり，出現範囲の中央部で相対的に大きくなった．しかし、変位分布は二つのピークがあることは変わらない．また，これまで確認されておらず，2014年の地震時にも活動していない伏在逆断層の存在も明らかにすることができた．

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  • Earthquake occurrence prediction model consideration one size small earthquake by active fault

    Grant number：16H03114  2016.04 - 2019.03

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (B)  Grant-in-Aid for Scientific Research (B)

    HIROUCHI DAISUKE

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    Grant amount：\16770000 （ Direct expense: \12900000 、 Indirect expense：\3870000 ）

    We conducted geological and geomophological survey around the Itoigawa-shizuoka tectonicline fault system located in the central part of Nagano prefecture, central Japan. In our study, it has revealed that the activity and segmentation of the ISTL active fault system based on the paleoseismological survey and the distribution of the tectonic landfom.

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  • Comprehensive Survey of 2015 Nepal Earthquake and Resulted Disasters

    Grant number：15H05793  2015.05 - 2016.03

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research Grant-in-Aid for Special Purposes  Grant-in-Aid for Special Purposes

    YATABE RYUICHI, FUKUOKA Hiroshi, HIGAKI Daisume, Bhandary N. P., HASEGAWA Shuichi, KAMIISHI Isao, IZUMI Kaoru, SATO Hiroshi, TAKAI Nobuo, KUMAHARA Yasuo, MIO Minoru, TAKADA Yosuke, TAKEUCHI Yasushi, OKUBO Takeyuki, MINAMI Makito, ATSUMI Tomohide, MURAKAMI Hitomi, YAGI Hiroshi, MOMOMURA Atsuko, YAMAGUCHI Satoru, KAWASHIMA Katsuhisa, HIRATA Nao, SAKAI Shinichi, KURASHIMO Eiji, KOKETSU Kazuki, SHIGEFUJI Michiko, ISHIYAMA Tatsuya, MATSUTA Nobuhisa, HIROUCHI Daisuke

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    Grant amount：\20600000 （ Direct expense: \20600000 ）

    In this study, we conducted a comprehensive investigation of the damage made by Nepal Gorkha Earthquake occurred on 25 April 2015. The main items of understandings of the investigation and analysis are: 1) earthquake occurrence mechanism , 2) mechanism of slope failures in the mountainous areas due to the earthquake and fault activities, 3) situation of damage and destruction of buildings and civil infrastructures, 4) situation analysis of earthquake-induced ice avalanche disaster, and 5) overall disaster risk assessment. Through these items of understanding, we contributed to second-stage disaster reduction and restoration plan preparation in Nepal.

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  • International Comparative Study on Mega-earthquake Disasters: Interactions in the Multi-layered Recovery Space

    Grant number：15H01905  2015.04 - 2019.03

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (A)  Grant-in-Aid for Scientific Research (A)

    Takahashi Makoto, Zikri Irfan, Nugroho Agus, Mahdi Saiful, Mardiatno Djati, Dyah Rahmawati Hizbaron, Estuning Tyas Wulan Mei, Meilano Irwan, Suhirman, Wu Guochun, Gao Mengtan, Zhao Yandong, Dalimunthe Syarifah Aini

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    Grant amount：\41730000 （ Direct expense: \32100000 、 Indirect expense：\9630000 ）

    This study points out that the post-disaster recovery itself brings about new kinds of disaster risk, related to the actores interactions in the recovery processes, that disaster experiences are not embedded into the community mechanisms for disaster risk reduction, and that these are caused by lack of vertical and horizontal coordination mechanisms in the post-disaster recovery processes, interrelated to pre- and post-disaster community and risk governances, through reformulation of the recovery model focusing on actors interactions in the multi-layered recovery space and comparison between recent three mega-earthquake disasters in humid Asia: the 2004 Sumatra, the 2008 Sichuan, and the 2011 Tohoku earthquake disasters.

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  • Geographical study toward enhancing ability of hazard maps for forecasting disaster and providing emergency information

    Grant number：15H02959  2015.04 - 2018.03

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (B)  Grant-in-Aid for Scientific Research (B)

    Suzuki Yasuhiro, YAMAOKA Kosyun, OKAMOTO Kohei, KUROKI Takahito, MATSUTA Nobuhisa, KUMAKI Yohta, ISHIGURO Satoshi, UNE Hiroshi, NAKAJIMA Hidetoshi, Yamaguchi Masaru

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    Grant amount：\17290000 （ Direct expense: \13300000 、 Indirect expense：\3990000 ）

    Hazard maps have been rapidly developed over the past 20 years. However, since the 2011 Great East Japan Earthquake, many problems have come to light each time a large-scale disaster occurs. Specific problems include, (1) variations in the definitions and concepts for each disaster type, (2) unmerged functions of "disaster prediction" and "evacuation information provision" for hazard maps, (3) insufficient spatial resolution of information corresponding to actual land conditions, and (4) excessive dependence on calculation results, without consideration of uncertainty. This study therefore aims to 1) systematically organize hazard maps, 2) advance disaster prediction maps, 3) strengthen the emergency information provision function, 4) contribute to disaster prevention geographical education, and 5) propose a comprehensive method of hazard map development from the viewpoint of geography.

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  • Feasibility study of terrestrial cosmogenic nuclides dating marine wave-cut benches uplifted by marine active faults

    Grant number：15K13577  2015.04 - 2018.03

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research Grant-in-Aid for Challenging Exploratory Research  Grant-in-Aid for Challenging Exploratory Research

    Ishiyama Tatsuya, ECHIGO Tomoo, YASUE Kenichi

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    Grant amount：\3770000 （ Direct expense: \2900000 、 Indirect expense：\870000 ）

    We carried out feasibility studies of terrestrial cosmogenic nuclides dating of abandoned ages of marine wave-cut benches caused by coseismic uplift events associated with faulting on marine active faults and subduction zone megathrusts. After through reviews of previous studies on coseismically uplifted marine terraces, geomorphic and geologic analyses on marine terraces and underlying bedrock types that effect on availability of this method, we successfully collected rock samples at two survey points along rocky coasts in the Sanriku area, Northeast Japan, where long-term and co-, post- and interseismic crustal movements were evidenced by Pleistocene and Holocene marine terraces, which are now under measurement procedures. This study shows terrestrial cosmogenic nuclides dating is a powerful tool for estimating timing of tectonic uplifts recorded by uplifted marine terraces, which eventually lead to full understanding of seismic potentials from otherwise hidden marine active faults.

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  • crustal deformation system non the active fault slip

    Grant number：25350427  2013.04 - 2018.03

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (C)  Grant-in-Aid for Scientific Research (C)

    Matta Nobuhisa

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    Grant amount：\5070000 （ Direct expense: \3900000 、 Indirect expense：\1170000 ）

    Crustal deformation observed by geodetic survey is the sum of elastic strain and permanent strain. The schedule at the start of the study was to focus on crustal movements around active faults. However, the 2014 Kamiro fault earthquake occurred. In the earthquake, a surface rupture appeared, but it was a smaller than a characteristic earthquake. This proved that there are multiple cases of earthquakes occurring along the active fault. It was also found that the crustal deformation observed by geodetic survey changes under the influence of the surrounding crustal movement event. The results of this research show that the crustal deformation in the island arc due to the slip of active fault is part of the whole deformation system and showed the necessity to consider the comprehensive crustal deformation process in the next step.

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  • Tectonic geomorphological studies on prediction of surface rupture patterns associated with active faulting

    Grant number：21300335  2009 - 2011

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (B)  Grant-in-Aid for Scientific Research (B)

    SUZUKI Yasuhiro, WATANABE Mitsuhisa, NAKATA Takashi, GOTO Hideaki, SUGITO Nobuhiko, KUMAHARA Yasuhiro, MATSUTA Nobuhisa, ISHIGURO Satoshi

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    Grant amount：\19890000 （ Direct expense: \15300000 、 Indirect expense：\4590000 ）

    Surface rupture patterns associated with active faulting reflect coseismic behavior of subsurface source faults, and thus tectonic geomorphology is a key to predict coseismic fault behavior. We examined relationships between coseismic surface ruptures and fault-related landforms related to the 1995 Neftegorsk, 1999 Chi-Chi, 1905 Bulnay, and 2008 Wenchuan earthquakes, in addition to the 1896 Rikuu, 1995 Hyogo-ken Nanbu, 2004 Chuetsu, 2007 Chuetsu-oki, and 2008 Iwate-Miyagi Nairiku earthquakes. In the case of Chi-Chi, spatial variation of coseismic displacement coincides with that of cumulative displacement, which would lead to long-term earthquake prediction, including earthquake magnitude and rupture directivity.

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  • 活断層に伴う地殻変形過程の研究

    Grant number：99J09951  1999 - 2001

    日本学術振興会  科学研究費助成事業 特別研究員奨励費  特別研究員奨励費

    松多 信尚

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    Grant amount：\2700000 （ Direct expense: \2700000 ）

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  • Geography Ⅰ （2023academic year） 3rd and 4th semester  - 水3～4

  • Seminar in Geography AⅠ （2023academic year） 1st semester  - その他

  • Seminar in Geography AⅡ （2023academic year） Second semester  - その他

  • Seminar in Geography BⅠ （2023academic year） 3rd and 4th semester  - その他

  • Seminar in Geography BⅡ （2023academic year） 3rd and 4th semester  - その他

  • Geographical Fieldwork　Ⅰ （2023academic year） 1st-4th semester  - その他

  • Geographical Fieldwork　Ⅱ （2023academic year） 1st-4th semester  - その他

  • Introduction to Topography Ⅰ （2023academic year） Third semester  - 火5～6

  • Introduction to Topography Ⅱ （2023academic year） Fourth semester  - 火5～6

  • Physical Geography Ⅰ （2023academic year） Third semester  - 火1～2

  • Physical Geography Ⅱ （2023academic year） Fourth semester  - 火1～2

  • Introduction to Physical Geography Ⅰ （2023academic year） Third semester  - 火1～2

  • Introduction to Physical Geography Ⅱ （2023academic year） Fourth semester  - 火1～2

  • Research Methods in Physical Geography （2023academic year） 1st and 2nd semester  - その他

  • Research Methods in Physical Geography （2023academic year） 1st and 2nd semester  - その他

  • Primary Education Social Studies Basic Content （2023academic year） 1st semester  - 水3～4

  • Primary Education Social Studies Basic Content （2023academic year） Second semester  - 水3～4

  • Primary Education Social Studies Content Teaching （2023academic year） 1st semester  - 水3～4

  • Primary Education Social Studies Content Teaching （2023academic year） Second semester  - 水3～4

  • Advanced Seminar on Earth and Planetary Sciences （2023academic year） Year-round  - その他

  • Geomathematical Sciences （2023academic year） Prophase  - その他

  • Seminar in Seismology （2023academic year） Year-round  - その他

  • Seminar in Teaching Profession Practice (Secondary school) （2023academic year） 1st-4th semester  - 水7～8

  • Special Studies in Idea and Problems of Academic Training B （2023academic year） 1st semester  - 金1,金2

  • Special Studies in Educational Science(Physical Geography IA): Seminar （2023academic year） 1st semester  - その他

  • Special Studies in Educational Science(Physical Geography IB): Seminar （2023academic year） Second semester  - その他

  • Special Studies in Educational Science(Physical Geography IIA): Seminar （2023academic year） Third semester  - 火7,火8

  • Special Studies in Educational Science(Physical Geography IIB): Seminar （2023academic year） Fourth semester  - 火7,火8

  • Special Studies in Educational Science(Physical Geography IA) （2023academic year） 1st semester  - その他

  • Special Studies in Educational Science(Physical Geography IB) （2023academic year） Second semester  - その他

  • Special Studies in Educational Science(Physical Geography IIA) （2023academic year） Third semester  - その他

  • Special Studies in Educational Science(Physical Geography IIB) （2023academic year） Fourth semester  - その他

  • Project Research in Educational Science （2023academic year） 1st-4th semester  - その他

  • An Introduction to the Physical Geography (1) （2023academic year） Third semester  - 火1～2

  • An Introduction to the Physical Geography (2) （2023academic year） Fourth semester  - 火1～2

  • Physical Geography Seminar A (1) （2023academic year） 1st semester  - その他

  • Physical Geography Seminar A (2) （2023academic year） Second semester  - その他

  • Physical Geography Seminar B (1) （2023academic year） 3rd and 4th semester  - その他

  • Physical Geography Seminar B (2) （2023academic year） 3rd and 4th semester  - その他

  • Senior Seminar in Liberal Studies （2023academic year） 1st-4th semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2023academic year） 1st semester  - 金5,金6

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2023academic year） Second semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2023academic year） Third semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2023academic year） Fourth semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2023academic year） 1st semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2023academic year） Second semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2023academic year） Third semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2023academic year） Fourth semester  - その他

  • Active Tectonics （2022academic year） Late  - その他

  • Secondary Education Social Studies Content Construction Ⅰ （2022academic year） 1st semester  - 火3,火4

  • Secondary Education Social Studies Content Construction Ⅱ （2022academic year） Second semester  - 火3,火4

  • Secondary Education Social Studies Content Construction Ⅲ （2022academic year） 1st semester  - 月1～2

  • Secondary Education Social Studies Content Construction Ⅳ （2022academic year） Second semester  - 月1～2

  • Seminar in Geography CⅠ （2022academic year） 1st semester  - その他

  • Seminar in Geography CⅡ （2022academic year） Second semester  - その他

  • Seminar in Geography DⅠ （2022academic year） 3rd and 4th semester  - その他

  • Seminar in Geography DⅡ （2022academic year） 3rd and 4th semester  - その他

  • Geographical Fieldwork　Ⅰ （2022academic year） 1st-4th semester  - その他

  • Geographical Fieldwork　Ⅱ （2022academic year） 1st-4th semester  - その他

  • Regional Geography AⅠ （2022academic year） 1st semester  - 木5～6

  • Regional Geography AⅡ （2022academic year） Second semester  - 木5～6

  • Physical Geography Ⅰ （2022academic year） Third semester  - 水3～4

  • Physical Geography Ⅱ （2022academic year） Fourth semester  - 水3～4

  • Research Methods in Physical Geography （2022academic year） 1st and 2nd semester  - その他

  • Research Methods in Physical Geography （2022academic year） 1st and 2nd semester  - その他

  • Content Studies in Social Studies for Elementary Education A (1) （2022academic year） 1st semester  - 木3,木4

  • Content Studies in Social Studies for Elementary Education A (2) （2022academic year） Second semester  - 木3,木4

  • Content Studies in Social Studies for Elementary Education B (1) （2022academic year） Third semester  - 木3,木4

  • Primary Education Social Studies Content Teaching （2022academic year） 1st semester  - 木3,木4

  • Primary Education Social Studies Content Teaching （2022academic year） Third semester  - 木3,木4

  • geomorphology （2022academic year） Second semester  - 木3～4

  • Geographical Fieldwork(1) （2022academic year） 1st-4th semester  - その他

  • Geographical Fieldwork(2) （2022academic year） 1st-4th semester  - その他

  • Regional Geography B (1) （2022academic year） 1st semester  - 木5～6

  • Regional Geography B (2) （2022academic year） Second semester  - 木5～6

  • Seminar in Seismology （2022academic year） Year-round  - その他

  • Approaches to Education （2022academic year） 1st semester  - 火1～2

  • Special Studies in Idea and Problems of Academic Training B （2022academic year） 1st semester  - 金1,金2

  • Special Studies in Educational Science(Physical Geography IA): Seminar （2022academic year） 1st semester  - その他

  • Special Studies in Educational Science(Physical Geography IB): Seminar （2022academic year） Second semester  - その他

  • Special Studies in Educational Science(Physical Geography IIA): Seminar （2022academic year） Third semester  - 火7,火8

  • Special Studies in Educational Science(Physical Geography IIB): Seminar （2022academic year） Fourth semester  - 火7,火8

  • Special Studies in Educational Science(Physical Geography IA) （2022academic year） 1st semester  - その他

  • Special Studies in Educational Science(Physical Geography IB) （2022academic year） Second semester  - その他

  • Special Studies in Educational Science(Physical Geography IIA) （2022academic year） Third semester  - 火5,火6

  • Special Studies in Educational Science(Physical Geography IIB) （2022academic year） Fourth semester  - 火5,火6

  • Project Research in Educational Science （2022academic year） 1st-4th semester  - その他

  • An Introduction to the Physical Geography (1) （2022academic year） Third semester  - 水3～4

  • An Introduction to the Physical Geography (2) （2022academic year） Fourth semester  - 水3～4

  • Physical Geography Seminar C (1) （2022academic year） 1st semester  - その他

  • Physical Geography Seminar C (2) （2022academic year） Second semester  - その他

  • Physical Geography Seminar D (1) （2022academic year） 3rd and 4th semester  - その他

  • Physical Geography Seminar D (2) （2022academic year） 3rd and 4th semester  - その他

  • Research Methods in Physical Geography (1) （2022academic year） 1st and 2nd semester  - その他

  • Research Methods in Physical Geography (2) （2022academic year） 1st and 2nd semester  - その他

  • disaster preparedness education （2022academic year） 1st semester  - 木1～2

  • Senior Seminar in Liberal Studies （2022academic year） 1st-4th semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2022academic year） 1st semester  - 金5,金6

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2022academic year） Second semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2022academic year） Third semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2022academic year） Fourth semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2022academic year） 1st semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2022academic year） Second semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2022academic year） Third semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2022academic year） Fourth semester  - その他

  • Active Tectonics （2021academic year） Late  - その他

  • Developmental Studies of Secondary Geography Education (1) （2021academic year） Fourth semester  - 木1～2

  • Developmental Studies of Secondary Geography Education (2) （2021academic year） Fourth semester  - 木3～4

  • Secondary Education Social Studies Content Construction Ⅰ （2021academic year） 1st semester  - 火3,火4

  • Secondary Education Social Studies Content Construction Ⅱ （2021academic year） Second semester  - 火3,火4

  • Secondary Education Social Studies Content Construction Ⅲ （2021academic year） 1st semester  - 月1～2

  • Secondary Education Social Studies Content Construction Ⅳ （2021academic year） Second semester  - 月1～2

  • Seminar in Geography AⅠ （2021academic year） 1st semester  - その他

  • Seminar in Geography AⅡ （2021academic year） Second semester  - その他

  • Seminar in Geography BⅠ （2021academic year） 3rd and 4th semester  - その他

  • Seminar in Geography BⅡ （2021academic year） 3rd and 4th semester  - その他

  • Geographical Fieldwork　Ⅰ （2021academic year） 1st-4th semester  - その他

  • Geographical Fieldwork　Ⅱ （2021academic year） 1st-4th semester  - その他

  • Regional Geography AⅠ （2021academic year） 1st semester  - 木5～6

  • Regional Geography AⅡ （2021academic year） Second semester  - 木5～6

  • Physical Geography Ⅰ （2021academic year） Third semester  - 水3～4

  • Physical Geography Ⅱ （2021academic year） Fourth semester  - 水3～4

  • Research Methods in Physical Geography （2021academic year） 1st and 2nd semester  - その他

  • Research Methods in Physical Geography （2021academic year） 1st and 2nd semester  - その他

  • Content Studies in Social Studies for Elementary Education A （2021academic year） 1st and 2nd semester  - 木3～4

  • Content Studies in Social Studies for Elementary Education A (1) （2021academic year） 1st semester  - 木3,木4

  • Content Studies in Social Studies for Elementary Education B (1) （2021academic year） Third semester  - 木3,木4

  • Primary Education Social Studies Content Teaching （2021academic year） 1st semester  - 木3,木4

  • Primary Education Social Studies Content Teaching （2021academic year） Third semester  - 木3,木4

  • Seminar in Physics of the Earth and Planetary Interior （2021academic year） Year-round  - その他

  • Geographical Fieldwork(1) （2021academic year） special  - その他

  • Geographical Fieldwork(2) （2021academic year） special  - その他

  • Regional Geography B (1) （2021academic year） 1st semester  - 木5～6

  • Regional Geography B (2) （2021academic year） Second semester  - 木5～6

  • Approaches to Education （2021academic year） 1st semester  - 火1～2

  • Special Studies in Idea and Problems of Academic Training B （2021academic year） 1st semester  - 金1,金2

  • Introduction of Project Based Learning （2021academic year） 1st semester  - 火1,火2

  • Special Studies in Educational Science(Physical Geography IA): Seminar （2021academic year） 1st semester  - 火7,火8

  • Special Studies in Educational Science(Physical Geography IB): Seminar （2021academic year） Second semester  - 火7,火8

  • Special Studies in Educational Science(Physical Geography IIA): Seminar （2021academic year） Third semester  - 火7,火8

  • Special Studies in Educational Science(Physical Geography IIB): Seminar （2021academic year） Fourth semester  - 火7,火8

  • Special Studies in Educational Science(Physical Geography IA) （2021academic year） 1st semester  - 火5,火6

  • Special Studies in Educational Science(Physical Geography IB) （2021academic year） Second semester  - 火5,火6

  • Special Studies in Educational Science(Physical Geography IIA) （2021academic year） Third semester  - 火5,火6

  • Special Studies in Educational Science(Physical Geography IIB) （2021academic year） Fourth semester  - 火5,火6

  • Project Research in Educational Science （2021academic year） 1st-4th semester  - その他

  • An Introduction to the Physical Geography (1) （2021academic year） Third semester  - 水3～4

  • An Introduction to the Physical Geography (2) （2021academic year） Fourth semester  - 水3～4

  • Physical Geography Seminar A (1) （2021academic year） 1st semester  - その他

  • Physical Geography Seminar A (2) （2021academic year） Second semester  - その他

  • Physical Geography Seminar B (1) （2021academic year） 3rd and 4th semester  - その他

  • Physical Geography Seminar B (2) （2021academic year） 3rd and 4th semester  - その他

  • Research Methods in Physical Geography (1) （2021academic year） 1st and 2nd semester  - その他

  • Research Methods in Physical Geography (2) （2021academic year） 1st and 2nd semester  - その他

  • Senior Seminar in Liberal Studies （2021academic year） 1st-4th semester  - その他

  • Project Based Learning I （2021academic year） Second semester  - 火1,火2

  • Project Based Learning II （2021academic year） Third semester  - 火1,火2

  • Project Based Learning III （2021academic year） Fourth semester  - 火1,火2

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2021academic year） 1st semester  - 金5,金6

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2021academic year） Second semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2021academic year） Third semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2021academic year） Fourth semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2021academic year） 1st semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2021academic year） Second semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2021academic year） Third semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2021academic year） Fourth semester  - その他

  • Active Tectonics （2020academic year） Late  - その他

  • Secondary Education Social Studies Content Construction Ⅰ （2020academic year） 1st semester  - 火3,火4

  • Secondary Education Social Studies Content Construction Ⅱ （2020academic year） Second semester  - 火3,火4

  • Physical Geography Ⅰ （2020academic year） Summer concentration  - その他

  • Physical Geography Ⅱ （2020academic year） Summer concentration  - その他

  • Content Studies in Social Studies for Elementary Education A (1) （2020academic year） 1st semester  - 木3,木4

  • Content Studies in Social Studies for Elementary Education A (2) （2020academic year） Second semester  - 木3,木4

  • Content Studies in Social Studies for Elementary Education B (1) （2020academic year） Third semester  - 木3,木4

  • Primary Education Social Studies Content Teaching （2020academic year） 1st semester  - 木3,木4

  • Primary Education Social Studies Content Teaching （2020academic year） Third semester  - 木3,木4

  • Seminar in Physics of the Earth and Planetary Interior （2020academic year） Year-round  - その他

  • Geographical Fieldwork(1) （2020academic year） special  - その他

  • Geographical Fieldwork(2) （2020academic year） special  - その他

  • Approaches to Education （2020academic year） 1st semester  - 火1,火2

  • Special Studies in Idea and Problems of Academic Training B （2020academic year） 1st semester  - 金1,金2

  • Introduction of Project Based Learning （2020academic year） 1st semester  - 火1,火2

  • Project Research in Educational Science （2020academic year） 1st-4th semester  - その他

  • An Introduction to the Physical Geography (1) （2020academic year） Summer concentration  - その他

  • An Introduction to the Physical Geography (2) （2020academic year） Summer concentration  - その他

  • Physical Geography Seminar D (1) （2020academic year） 3rd and 4th semester  - その他

  • Physical Geography Seminar D (2) （2020academic year） 3rd and 4th semester  - その他

  • Research Methods in Physical Geography (1) （2020academic year） 1st and 2nd semester  - その他

  • Research Methods in Physical Geography (2) （2020academic year） 1st and 2nd semester  - その他

  • Senior Seminar in Liberal Studies （2020academic year） 1st-4th semester  - その他

  • Project Based Learning I （2020academic year） Second semester  - 火1,火2

  • Project Based Learning II （2020academic year） Third semester  - 火1,火2

  • Project Based Learning III （2020academic year） Fourth semester  - 火1,火2

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2020academic year） 1st semester  - 金5,金6

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2020academic year） Second semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2020academic year） Third semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2020academic year） Fourth semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2020academic year） 1st semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2020academic year） Second semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2020academic year） Third semester  - その他

  • Special Studies in Educational Science(Special Studies in Project Based Learning （2020academic year） Fourth semester  - その他

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Social Activities

  • 西日本豪雨から四年、災害伝承碑をみて思うこと ー西日本豪雨から四年後に思うことー

    Role(s)：Contribution

    (公財)岡山県郷土文化財団  きび野 

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    Type：Promotional material

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Media Coverage

  • 「人文地理学からみる世界」第9回 （１学期） TV or radio program

    放送大学  2022.5

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Academic Activities

  • The General Meeting of the AJG Autumn 2021

    Role(s)：Planning, management, etc.

    2020.9 - 2021.10

    　More details

    Type：Academic society, research group, etc. 

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