Faculty Profiles - MATTA Nobuhisa

MISC - MATTA Nobuhisa

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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

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

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

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

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

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

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

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

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

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

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

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.

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

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

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

Web of Science

J-GLOBAL

researchmap

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

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)

Web of Science

J-GLOBAL

researchmap

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

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

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

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

Surface deformation caused by the northern part of Nagano earthquake

9 - 15 2012.1

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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