| Project/Area Number |
12480019
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| Research Category |
Grant-in-Aid for Scientific Research (B)
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| Allocation Type | Single-year Grants |
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| Section | 一般 |
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| Research Field |
自然地理学
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| Research Institution | KYOTO UNIVERSITY |
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Principal Investigator |
OKADA Atsumasa Kyoto University, Graduate School of Science, Professor, 大学院・理学研究科, 教授 (90086174)
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| Co-Investigator(Kenkyū-buntansha) |
FUKUDA Yoichi Kyoto University, Graduate School of Science, Associate Professor, 大学院・理学研究科, 助教授 (30133854)
TSUTSUMI Hiroyuki Kyoto University, Graduate School of Science, Assistant Professor, 大学院・理学研究科, 助手 (60284428)
TAKEMURAME Keiji Kyoto University, Graduate School of Science, Professor, 大学院・理学研究科, 教授 (00201608)
TODA Shigeru Aichi University of Education, Faculty of Education, Associate Professor, 教育学部, 助教授 (40293732)
ITO Yasuto Osaka Prefectural University, Faculty of General Sciences, Associate Professor, 総合科学部, 助教授 (20285315)
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| Project Period (FY) |
2000 – 2002
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| Project Status |
Completed (Fiscal Year 2002)
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| Budget Amount *help |
¥15,700,000 (Direct Cost: ¥15,700,000)
Fiscal Year 2002: ¥1,700,000 (Direct Cost: ¥1,700,000)
Fiscal Year 2001: ¥4,200,000 (Direct Cost: ¥4,200,000)
Fiscal Year 2000: ¥9,800,000 (Direct Cost: ¥9,800,000)
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| Keywords | large scale alluvial plain / subsurface structure / active fault / seismic reflection survey / gravity measurement / drilling (bore-hole) core / precise measurement of carbon 14 |
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| Research Abstract |
The result of this scientific research is summarized as as below
Studies on the first-class active faults along the margin of the several large-scale alluvial plains were carried out for clarifying their fault topography and subsurface structure. There are Yoro-Kuwana fault system along the western margin of Nohbi plain, Katagihara fault along the margin of Kyoto basin, Komatubara fault along the southwestern margin of Nagano basin, Ikoma fault in the northeastern margin of Osaka plain, active fault belt along the western shore of Lake Biwa, Median Tectonic Line Fault system (Tokushima plain), submarine faults along the southern margin of the Japan Sea, northern Los Angels fault system in Los Angels basin and so on
We have carried out geomorphological survey, geophysical prospecting, drilling, trench excavation, and collected the information on deformation mode and subsurface structure along the major active faults, displacement rate and age for fault activity. Especially, sampling by using geoslicer and continuous analysis for these cores have clarified the most recent activity, reccurrence interval and slip rate, etc
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