Understanding of slow and ordinary earthquakes in a single framework of modeling
Project/Area Number |
21540429
|
Research Category |
Grant-in-Aid for Scientific Research (C)
|
Allocation Type | Single-year Grants |
Section | 一般 |
Research Field |
Solid earth and planetary physics
|
Research Institution | The University of Tokyo |
Principal Investigator |
|
Project Period (FY) |
2009 – 2011
|
Project Status |
Completed (Fiscal Year 2011)
|
Budget Amount *help |
¥3,120,000 (Direct Cost: ¥2,400,000、Indirect Cost: ¥720,000)
Fiscal Year 2011: ¥780,000 (Direct Cost: ¥600,000、Indirect Cost: ¥180,000)
Fiscal Year 2010: ¥1,040,000 (Direct Cost: ¥800,000、Indirect Cost: ¥240,000)
Fiscal Year 2009: ¥1,300,000 (Direct Cost: ¥1,000,000、Indirect Cost: ¥300,000)
|
Keywords | 地震現象 / 非線形系 / 地震 / スロースリップ / 断層 / 多孔質媒質 / 微動 / 熱多孔質媒質 / 流体 / 摩擦 / 空隙 |
Research Abstract |
We successfully simulate slow and ordinary earthquake in a single framework of modeling. It has become clear that key elements in the simulation are effects of fluid flow on fault slip and pore creation on the fault. We found that slower fault growth is obtained if we assume smaller permeabilities or larger pore creation rates. We also found that nonvolcanic tremor can be simulated if pore creation rate is large enough. Our calculation actually shows that fluid flow parallel to a fault must be assumed to simulate backward migration speeds of tremors on the order of 10-100km/h.
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Report
(4 results)
Research Products
(11 results)