In 1997, Akita Prefectural Government conducted a deep seismic reflection experiment to investigate an active fault zone developed along the eastern boundary of the Yokote Basin. We deployed additional thirty-six temporal seismic stations to record five dynamite shots for this experiment for the purpose of a refraction/wide-angle reflection crustal study. Our data provide important constraints on the velocity structure including lateral heterogeneity due to the fault system. This paper outlines our observations together with travel-times and record sections.
雑誌名
東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo
巻
74
号
1
ページ
49 - 62
発行年
1999-10-29
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
千屋断層帯における人工地震観測
ji0741002.pdf
(811.62KB)
