Grant-in-Aid for Co-operative Research (A)
|Allocation Type||Single-year Grants|
|Research Institution||Aichi Prefectural University|
OKADA Atsumasa Aichi Prefectural University, Department of Literature, Professor, 文学部, 教授 (90086174)
池田 安隆 東京大学, 理学部, 講師 (70134442)
今泉 俊文 山梨大学, 教育学部, 助教授 (50117694)
米倉 伸之 東京大学, 理学部, 教授 (30011563)
太田 陽子 横浜国立大学, 教育学部, 教授 (80017714)
松田 時彦 東京大学, 地震研究所, 教授 (70012896)
中田 高 広島大学, 文学部, 助教授 (60089779)
千田 昇 大分大学, 教育学部, 教授 (90111236)
|Project Fiscal Year
1989 – 1991
Completed(Fiscal Year 1991)
|Budget Amount *help
¥14,500,000 (Direct Cost : ¥14,500,000)
Fiscal Year 1991 : ¥4,400,000 (Direct Cost : ¥4,400,000)
Fiscal Year 1990 : ¥4,000,000 (Direct Cost : ¥4,000,000)
Fiscal Year 1989 : ¥6,100,000 (Direct Cost : ¥6,100,000)
|Keywords||Active fault / Trenching / Seismic profiling / Excavation study / Fault activity / Recurrence interval / Neodani fault / Median Tectonic Line / 発掘調査 / 有馬ー高槻構造線 / 花折断層 / 利府ー長町線 / 水縄断層 / 活断層詳細図 / 海底活断層 / 断層ストリップマップ / 千屋断層 / 北武断層 / 伊那谷断層系 / 有馬-高槻断層系 / 長府-長町断層系|
The precise seismic profilings have carried out at the Seto Inland Sea, Ariake-kai, Yatsushiro-kai and Mikawa Bay etc., where detailed characteristics of submarine active faults have been clarified. Sediments were sampled at the some parts of these seas using sea bottom drilling and piston corerer, and their fault activity and character were analysed by the sedimentological and dating methods.
The distribution of active faults beneath the deep seas such as Nankai Trough and Japan Trench has been mapped and compiled in the book entitled with -Active fault in Japan : revised edition" published from the University of Tokyo Press in 1991. This comprehensive book was edited by almost all researchers of this project, and aims to display many data of active faults in the form of sheet maps on the scale of 1 : 200, 000.
The excavation study for the Median Tectonic Line active fault system has been aimed principally at revealing ages of faulting event and recurrence intervals at three localities
in the eastern part of Shikoku. Especially, the latest event were extensively investigated and a probable candidate like ly seems to be 1596 Keicho earthquake (M=7.5).
Many drilling surveys were carried out along the Umehara fault belonging to the Nobi fault system and the Kitatake fault. The activity and behaviors of faulting for these active faults were clarified by investigating the lithology and dating for the core samples obtained. The displacements during the Nobi earthquake has reexamined along the Neodani fault, and its activity during the late Quaternary has been clarified with relation to the terrace choronology.
Detailed traces and classification of active fault along the major active faults were drawn on the large scale maps (scale /1 : 25, 000-1 : 10, 000) by photo-interpretation and field survey at the southern foot area of the Rokko Mountains and the western marginal area of the Kitakami River.
The ^<14>C dating method by accelerator mass spectrometry has been improved for evaluating the fault activity and past events of faulting. Less