Faculty Profiles - MATTA Nobuhisa

MISC - MATTA Nobuhisa

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糸魚川-静岡構造線岡谷断層・諏訪湖南岸断層と諏訪湖の成立ち—総特集糸魚川-静岡構造線断層帯

松多信尚

地図中心 ( 626 ) 40 - 43 2024.11

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その１

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自然災害科学総合シンポジウム講演論文集 61 1 - 16 2024.9

Language：Japanese Publisher：京都大学防災研究所自然災害研究協議会

2020年末から地殻変動を伴う群発地震活動が継続する能登半島北東部では，2023年5月5日にマグニチュード6.5（最大震度6強）の地震が発生し，さらに2024年1月1日にはマグニチュード7.6(最大震度7)の地震が発生した。この一連の地震活動の発生メカニズムおよびその災害像や地域社会・地域経済への影響を明らかにするために，令和5年度科学研究費助成事業（特別研究促進費）による総合調査として，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，震災被害調査，地域社会影響調査，津波調査，地域経済・復興過程影響調査を実施している。
主催：京都大学防災研究所自然災害研究協議会; 共催：千葉大学; 日程：2024年9月21日（土）終日（9時30分〜13時00分予定）; 場所：千葉大学西千葉キャンパスけやき会館大ホールハイブリッド開催
科学研究費補助金・特別研究促進費による突発災害調査研究令和5年度報告

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Pictorials Coastal changes associated with the 2024 Noto Peninsula Earthquake

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

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

令和6年能登半島地震に伴う海岸変化

安江健一, 立石良, 石山達也, 松多信尚, 廣内大助, 白濱吉起

第四紀研究 / 日本第四紀学会編 63 ( 2 ) 8 - 10 2024.5

Creativity and Assessment in Arts Education: Individual Differences in Creative Activities

185 105 - 113 2024.2

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

平松, 良浩, 蔵下, 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, 岩田, 知孝, 大堀, 道広, 村田, 晶

自然災害科学総合シンポジウム講演論文集 60 12 - 17 2023.9

Language：Japanese Publisher：京都大学防災研究所自然災害研究協議会

能登半島北東部では，2020年12月頃から地震数の顕著な増加と局所的な非定常地殻変動が観測され，活発な地震活動が継続する中，2022年6月19日にマグニチュード5.4（最大震度6弱）の地震が発生した。この長期間継続する地震活動や地殻変動の原因及び2022年6月19日の地震による災害像を明らかにするため，令和4年度科学研究費（特別研究促進費）による総合調査により，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，強震観測を実施した。
主催：京都大学防災研究所自然災害研究協議会; 日程：令和5年9月25日（月）13時00分～16時40分（終了予定）; 場所：きはだホール（京都大学宇治キャンパス内）およびZoomによるハイブリッド開催
科学研究費補助金・特別研究促進費による突発災害調査研究令和4年度報告

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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

越境する創造性の育成（3）—芸術教科の創造性をいかに評価するか

小川容子, 徳田旭昭, 大月ヒロ子, 松多信尚, 清田哲男

日本教育心理学会総会発表論文集 65 68 - 69 2023

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

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

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

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

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 ( 38・39 ) 315 - 323 2021.11

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

CiNii Books

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Other Link： https://ndlsearch.ndl.go.jp/books/R000000004-I032825749

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

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

Language：Japanese Publisher：The Association of Japanese Geographers

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."

DOI： 10.14866/ajg.2021s.0_148

CiNii Article

J-GLOBAL

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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

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

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

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

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

MATSUTA NOBUHISA

Proceedings of the General Meeting of the Association of Japanese Geographers 2021s 148 2021

Language：Japanese Publisher：The Association of Japanese Geographers

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."

DOI： 10.14866/ajg.2021s.0_148

CiNii Article

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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

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

Language：Japanese Publisher：The Association of Japanese Geographers

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.

DOI： 10.14866/ajg.2020a.0_143

CiNii Article

J-GLOBAL

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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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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.

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

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

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

Language：English Publisher：SPRINGEROPEN

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.

DOI： 10.1186/s40623-018-0890-9

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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

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

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

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

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

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

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

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

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

Language：English Publisher：SPRINGER

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

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

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

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

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

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

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

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

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

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

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

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

Language：English Publisher：SPRINGER HEIDELBERG

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

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

Language：English Publisher：The Remote Sensing Society of Japan

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). 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. 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

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

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

Language：Japanese Publisher：The Association of Japanese Geographers

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.

DOI： 10.4157/ejgeo.11.526

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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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

Language：Japanese Publisher：Japanese Society for Active Fault Studies

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.

DOI： 10.11462/afr.2015.43_109

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

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

Language：Japanese Publisher：Japanese Society for Active Fault Studies

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.

DOI： 10.11462/afr.2015.43_149

What Differentiated Local Casualties Caused by the Tsunami ?

TAKAHASHI Makoto, MATSUTA Nobuhisa

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

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

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

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—Meiji Sanriku (1896 A.D.), Syowa Sanriku (1933 A.D.), and Chilean Sanriku (1960 A.D.) tsunamis—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

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

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

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

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

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

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

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

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

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

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

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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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

Language：Japanese Publisher：The Association of Japanese Geographers

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

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

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

Language：English

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.

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

Publisher：The Association of Japanese Geographers

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 “Web-GIS based active fault information system for the Itoi-gawa-Shizuoka Tectonic Line”. 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

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 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. 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

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

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

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

Language：Japanese Publisher：Tokyo Geographical Society

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. 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. 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

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

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

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

81 ( 2 ) 97 - 106 2006

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

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

Language：Japanese Publisher：Japanese Society for Active Fault Studies

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. 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

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

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

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

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

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

Language：Japanese Publisher：Japanese Society for Active Fault Studies

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

Language：Japanese Publisher：Japanese Society for Active Fault Studies

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

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

Language：Japanese Publisher：The Geodetic Society of Japan

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

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

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

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

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

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

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

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

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

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

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

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. 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

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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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