| Project/Area Number |
61540291
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| Research Category |
Grant-in-Aid for General Scientific Research (C)
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| Allocation Type | Single-year Grants |
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| Research Field |
固体地球物理学
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| Research Institution | KYOTO UNIVERSITY |
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Principal Investigator |
ANDO Masataka Kyoto Univ.DPRI Research Associate, 防災研究所, 助手 (80027292)
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| Co-Investigator(Kenkyū-buntansha) |
HIRAHARA Kazuro Kyoto Univ.DPRI Research Associate, 防災研究所, 助手 (40165197)
OIKE Kazuo Kyoto Univ.DPRI Associate Prof., 防災研究所, 助教授 (40027248)
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| Project Period (FY) |
1986 – 1987
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| Project Status |
Completed (Fiscal Year 1987)
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| Budget Amount *help |
¥1,900,000 (Direct Cost: ¥1,900,000)
Fiscal Year 1987: ¥400,000 (Direct Cost: ¥400,000)
Fiscal Year 1986: ¥1,500,000 (Direct Cost: ¥1,500,000)
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| Keywords | Shear-wave polarization / stress change / seismic observation / S波偏光異方性 / 異方性, 地殻応力変化 / 地震波観測, クラック |
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| Research Abstract |
We have identified shear-wave splitting, diagnostic of the effective anisotropy induced by aligned microcrackes, in the wavetrains of micro-earthquakes at many seismic stations in Japan.
In the Kinki districts, we find that the directions of polarization of the faster split shear-waves are nearly parallel for all azimuths of arrivals, and for all angles of incidence less than the critical amgle at three of four stations of Abuyama Seismological Observatory, Kyoto University. These directions of polarization are consistent with the axis of maximum compression obtained from earthquake fault-plane mechanisms, and also agree with the directions of the general trends of geological structures which represent the orientations of the cleavage or lamination. These results suggest that crack-induced anisotropy is present in the brittle upper crust beneath Japan, as has been found elsewhere, but we could not distinguish whether this reflects the distributions of cracks induced by the present stress field, or results from the general trends of surface geology. Although the delay times between faster and slower shear waves are difficult to estimate reliably, because of their high sensitivity to internal interfaces, the delay times can be interpreted as the result of a distribution of parallel vertical cracks with a crack density of about 0.04. The consistency or lack of consistency of the directions of the shear-wave polarizations at four stations demonstrates the effects surface topography and near surface layring on the shear-wave polarizations.
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