Reconstruction of the AD818 Earthquake by tectonic geomorphology, late Quaternary geology and archaeology
Project/Area Number |
26350401
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Research Category |
Grant-in-Aid for Scientific Research (C)
|
Allocation Type | Multi-year Fund |
Section | 一般 |
Research Field |
Geography
|
Research Institution | Hiroshima University |
Principal Investigator |
|
Project Period (FY) |
2014-04-01 – 2017-03-31
|
Project Status |
Completed (Fiscal Year 2016)
|
Budget Amount *help |
¥4,810,000 (Direct Cost: ¥3,700,000、Indirect Cost: ¥1,110,000)
Fiscal Year 2016: ¥130,000 (Direct Cost: ¥100,000、Indirect Cost: ¥30,000)
Fiscal Year 2015: ¥2,860,000 (Direct Cost: ¥2,200,000、Indirect Cost: ¥660,000)
Fiscal Year 2014: ¥1,820,000 (Direct Cost: ¥1,400,000、Indirect Cost: ¥420,000)
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Keywords | 活断層 / 関東地方 / 変動地形 / 平安時代 / 関東平野 |
Outline of Final Research Achievements |
The unsolved paleoseismological problem in the northern Kanto district, central Japan is that an active fault generating a great earthquake in A.D. 818 recorded by the historical formal record has not been identified. In the northwestern part of the Kanto Plain, it is well known that paleo-liquefactions, fissures or landslides due to strong shaking are observed in more than 50 archeological sites. I tried geological and geomorphological survey with collecting archaeological data related to strong shaking during A. D. 818. Based on trenching survey, I suggested that Ota fault could be a fault corresponding to the 818 earthquake.
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Report
(4 results)
Research Products
(7 results)