A study on dynamic rupture process of an asperity and radiation of short-period seismic waves
| Project/Area Number |
20540407
|
|---|
| 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 |
KATO Naoyuki The University of Tokyo, 地震研究所, 准教授 (60224523)
|
|---|
| Co-Investigator(Kenkyū-buntansha) |
宮武 隆 東京大学, 地震研究所, 准教授 (60126183)
中原 恒 東北大学, 大学院・理学研究科, 助教 (20302078)
|
|---|
| Project Period (FY) |
2008 – 2010
|
| Project Status |
Completed (Fiscal Year 2010)
|
| Budget Amount *help |
¥2,080,000 (Direct Cost: ¥1,600,000、Indirect Cost: ¥480,000)
Fiscal Year 2010: ¥780,000 (Direct Cost: ¥600,000、Indirect Cost: ¥180,000)
Fiscal Year 2009: ¥650,000 (Direct Cost: ¥500,000、Indirect Cost: ¥150,000)
Fiscal Year 2008: ¥650,000 (Direct Cost: ¥500,000、Indirect Cost: ¥150,000)
|
|---|
| Keywords | 地震現象 / アスペリティ / 短周期地震波 / シミュレーション / エンベロープ / 応力集中 / 応力降下量 |
|---|
| Research Abstract |
We investigate effects of stress concentration at the rim of an asperity due to surrounding aseismic sliding through numerical simulations. The stress concentration due to aseismic sliding promotes earlier occurrence of seismic rupture. This results in lower average stress drop of earthquake. This effect of stress concentration at the rim of asperity may explain the difference in average stress drop between intraplate and interplate earthquakes. The stress concentration at the edge of an asperity affects rupture process of asperity, and the average stress drop of asperity rupture increases with fracture energy or critical slip-weakening distance. A numerical simulation is conducted for dynamic rupture process of a circular asperity, where stress concentration is generated at the rim of the asperity. Seismic rupture starts from a point of the stress concentrated rim and propagates bilaterally around the rim. A significant slip pulse is generated at the end of the rupture due to rupture front focusing. We compile spatial distributions of short-period seismic energy radiation on faults estimated from the envelope inversion method to obtain the scaling law, frequency dependence of seismic energy radiation, and locality.
|
Report
(4 results)
Research Products
(13 results)
