| Project/Area Number |
06402016
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| Research Category |
Grant-in-Aid for Scientific Research (A)
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| Allocation Type | Single-year Grants |
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| Section | 一般 |
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| Research Field |
固体地球物理学
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| Research Institution | University of Tokyo |
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Principal Investigator |
OKUBO Shuhei University of Tokyo, Earthquake Research Institute, Associate Professor, 地震研究所, 助教授 (30152078)
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| Co-Investigator(Kenkyū-buntansha) |
YOSHIDA Shigeo University of Tokyo, Earthquake Research Institute, Research Associate, 地震研究所, 助手 (50262085)
TSUBOI Seiji National Defense Academy, Department of Geoscience, Associate Professor, 地球科学科, 助教授 (90183871)
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| Project Period (FY) |
1994 – 1996
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| Project Status |
Completed (Fiscal Year 1996)
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| Budget Amount *help |
¥17,600,000 (Direct Cost: ¥17,600,000)
Fiscal Year 1996: ¥1,700,000 (Direct Cost: ¥1,700,000)
Fiscal Year 1995: ¥2,900,000 (Direct Cost: ¥2,900,000)
Fiscal Year 1994: ¥13,000,000 (Direct Cost: ¥13,000,000)
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| Keywords | Geoid / Fault Motion / Altimetry / Satellite / Slow Earthquake / Silent Earthquake / Silent Earhquake |
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| Research Abstract |
We have detected a significant subsidence of the sea level of the Pacific near the coast of Peru and Chile after the 1994 Bolivia earthquake by analyzing the TOPEX/POSEIDON satellite altimetry data. The isotropic pattern of the sea surface change indicates the existence of isotropic implosion source with time scale of less than 10 days. This finding provides the evidence for the phase change of mantle minerals as a critical factor for deep earthquakes.
We presented a theory for displacement caused by a point dislocation in a radially heterogeneous spherical earth. The objective of this research was to constrain the fault model of the 1994 Bolivia earthquake by using GPS observations on the Pacific coast of the South American continent.
In order to achieve well constrained fault model, we investigate the possibility of using absolute gravity values which complement the geoid height change. For that purpose, we verified the 1 microgal precision of the new generation absolute gravimeter FG5 by collocation with superconducting gravimeters.
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