Faculty Profiles - MATTA Nobuhisa

MISC - MATTA Nobuhisa

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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

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.

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

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

Language：Japanese Publisher：Japanese Society for Active Fault Studies

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

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

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

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

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

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

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

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

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

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

Language：Japanese Publisher：Japanese Society for Active Fault Studies

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

Language：Japanese Publisher：Japanese Society for Active Fault Studies

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

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

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

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

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

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

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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