The Tokachi Basin, the second largest sedimentary basin on the Japanese islands, is located in the hinterland of the Hidaka Collision zone, Hokkaido. The eastern part of the basin is bounded by the NS trending Tokachi active fault system, which is an east-dipping reverse fault system. In 1999, an extensive seismic reflection survey was undertaken across this basin, from which inportant information on the shallow part of the basin structure was obtained. This paper presents the seismological structure from the refraction analysis with its preliminary geological interpretation.
雑誌名
東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo
巻
77
号
2
ページ
131 - 138
発行年
2002-12-27
ISSN
00408972
書誌レコードID
AN00162258
フォーマット
application/pdf
日本十進分類法
453
出版者
東京大学地震研究所
出版者別名
Earthquake Research Institute, University of Tokyo
稠密展開屈折法探査による十勝構造盆地浅部構造の解明
ji0772005.pdf
(1.39MB)
