Seismological and geological characterization of the crust in the southern part of northern Fossa Magna, central Japan
-
- Sato Hiroshi
- Earthquake Research Institute, University of Tokyo
-
- Iwasaki Takaya
- Earthquake Research Institute, University of Tokyo
-
- Ikeda Yasutaka
- Department of Earth and Planetary Science
-
- Takeda Tetsuya
- Earthquake Research Institute, University of Tokyo
-
- Matsuta Nobuhisa
- Earthquake Research Institute, University of Tokyo
-
- Imai Tomoko
- Earthquake Research Institute, University of Tokyo
-
- Kurashimo Eiji
- Earthquake Research Institute, University of Tokyo
-
- Hirata Naoshi
- Earthquake Research Institute, University of Tokyo
-
- Sakai Sin'ichi
- Earthquake Research Institute, University of Tokyo
-
- Elouai Driss
- Department of Earth and Planetary Systems Science, Hiroshima University
-
- Kawanaka Taku
- JGI Inc.
-
- Kawasaki Shinji
- JGI Inc.
-
- Abe Susumu
- JGI Inc.
-
- Kozawa Takeshi
- JGI Inc.
-
- Ikawa Takeshi
- JGI Inc.
-
- Arai Yoshimasa
- Tokyo Electric Power Company
-
- Kato Naoko
- Earthquake Research Institute, University of Tokyo
この論文をさがす
抄録
The northern Fossa Magna (NMF) is a Miocene rift basin formed in the final stages of the opening of the Sea of Japan. The northern part of Itoigawa-Shizuoka Tectonic Line (ISTL) bounds the western part of the NMF and forms an active fault system that displays one of the largest slip rates in the Japanese islands. Reflection and refraction/wide-angle reflection profiling and earthquake observations by a dense array were undertaken across the northern part of ISTL in order to delineate structures in the crust, and deep geometry of the active fault systems. The ISTL active fault system at depth (ca. 2 km) shows east-dipping low-angle in Omachi and Matsumoto and is extended beneath the Central Uplift Zone and Komoro basin keeping the same dip-angle down to ca. 15 km. The upper part of the crust beneath the Central Uplift Zone is marked by the high Vp and high resistivity zone. Beneath the folded zone of the NMF, the middle to lower crust shows low Vp, low resistivity and more reflective features. The balanced geologic cross-section based on the reflection profiles suggests that the shortening deformation since the late Neogene was produced by the basin inversion of the Miocene low-angle normal fault.
収録刊行物
-
- Earth, Planets and Space
-
Earth, Planets and Space 56 (12), 1253-1259, 2004
地球電磁気・地球惑星圏学会 、公益社団法人 日本地震学会、特定非営利活動法人 日本火山学会、日本測地学会、日本惑星科学会
- Tweet
キーワード
詳細情報 詳細情報について
-
- CRID
- 1390282681489285248
-
- NII論文ID
- 10017467138
- 130003781018
-
- NII書誌ID
- AA11211921
-
- ISSN
- 18805981
- 13438832
-
- NDL書誌ID
- 7279571
-
- 本文言語コード
- en
-
- データソース種別
-
- JaLC
- NDL
- Crossref
- CiNii Articles
- KAKEN
-
- 抄録ライセンスフラグ
- 使用不可