研究者詳細 - 松多　信尚

MISC - 松多　信尚

分割表示 203 件中 161 - 180 件目／全件表示 >>

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年

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年

横手盆地東縁断層帯・千屋断層の形成過程と千屋丘陵の活構造

楮原京子, 今泉俊文, 宮内崇裕, 佐藤比呂志, 内田拓馬, 越後智雄, 石山達也, 松多信尚, 岡田真介, 池田安隆, 戸田茂, 越谷信, 野田賢, 加藤一, 野田克也, 三輪敦志, 黒澤英樹, 小坂英輝, 野原壯

地學雜誌 115 ( 6 ) 691 - 714 2006年12月

記述言語：日本語出版者・発行元：公益社団法人東京地学協会

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

DOI： 10.5026/jgeography.115.6_691

17. 台湾西部山麓地域における1999年9月の集集地震で生じた滝の後退速度(日本地形学連合2005年秋季大会)

早川裕一, 松多信尚, 松倉公憲

地形 27 ( 1 ) 107 - 107 2006年

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年

千屋断層（花岡）を横断する浅層反射法地震探査: データ取得と処理について

佐藤比呂志, 池田安隆, 今泉俊文, 三ヶ田均, 戸田茂, 堤浩之, 越谷信, 野田賢, 伊藤谷生, 宮内崇裕, 八木浩司, 東郷正美, 岩崎貴哉, 坂守, 平田直, 松多信尚, 河村知徳, 石丸恒存, 井川猛, 千屋96反射法地震探査グループ

東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo 81 ( 2 ) 97 - 106 2006年

横手盆地東縁断層帯・太田断層を横断する浅層反射法地震探査(2003年):データ取得と処理について (特集反射法地震探査による活断層の地下形状(Part1))

楮原京子, 内田拓馬, 宮内崇裕, 今泉俊文, 佐藤比呂志, 越後智雄, 池田安隆, 越谷信, 野田賢, 松多信尚, 石山達也, 戸田茂, 加藤一, 岡田真介, 加藤直子, 荻野スミ子, 木村治夫, 渡邉勇二, 宇野知樹, 田中環, 小島淳, 市川史大, 小畑一馬, 乗田康之, 今村朋裕, 野田克也, 井川猛

東京大学地震研究所彙報 81 ( 2 ) 107 - 117 2006年

糸魚川-静岡構造線断層帯北部,大町～松本北部間の変動地形認定と鉛直平均変位速度解明

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

活断層研究 2006 ( 26 ) 121 - 136 2006年

記述言語：日本語出版者・発行元：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.<BR>One of the remarkable results by using this data set is a large number of, here 84, photogrammetrically measured landform transections to quantify the tectonic deformations. We could calculate vertical slip rates of the faults at 74 points, based on the estimated ages of terraces (H: 120 kyrs, M: 50-100 kyrs, Ll: 10-20 kyrs, L2: 4-7 kyrs, L3: 1-2 kyrs). The vertical slip rates distributed in the northern part of the study area show 0.2-5.5 mm/yr on the L terraces (less than 20 kyrs) and 0.05-0.9 mm/yr on the M and H terraces (more than 50 kyrs). The vertical slip rates of the faults located in the central and southern part of the study area are 0.2-3.1 mm/yr.

DOI： 10.11462/afr1985.2006.26_121

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横手盆地東縁断層帯・千屋断層（運上野）を横断する浅層反射法地震探査（2004年） : データ取得と処理について

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

東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo 81 ( 2 ) 119 - 128 2006年

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年

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年

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年

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年

国府津-松田断層帯松田北断層における浅層反射法地震探査

木村治夫, 荻野スミ子, 楮原京子, 小田晋, 野田克也, 井川猛, 佐藤比呂志, 伊藤谷生, 宮内崇裕, 松多信尚, 河村知徳, 石山達也, 岡田真介, 加藤直子

活断層研究 2005 ( 25 ) 85 - 92 2005年

記述言語：日本語出版者・発行元：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年