| Project/Area Number |
23654170
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| Research Category |
Grant-in-Aid for Challenging Exploratory Research
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| Allocation Type | Multi-year Fund |
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| Research Field |
Geology
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| Research Institution | Akita University |
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Principal Investigator |
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| Co-Investigator(Kenkyū-buntansha) |
OTSUKI Kenshiro 東北大学, 理学研究科, 名誉教授 (70004497)
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| Co-Investigator(Renkei-kenkyūsha) |
MUTO Jun 東北大学, 理学研究科, 助教 (40545787)
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| Project Period (FY) |
2011 – 2012
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| Project Status |
Completed (Fiscal Year 2012)
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| Budget Amount *help |
¥3,640,000 (Direct Cost: ¥2,800,000、Indirect Cost: ¥840,000)
Fiscal Year 2012: ¥910,000 (Direct Cost: ¥700,000、Indirect Cost: ¥210,000)
Fiscal Year 2011: ¥2,730,000 (Direct Cost: ¥2,100,000、Indirect Cost: ¥630,000)
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| Keywords | 断層 / 固着すべり / 応力場 / ガス圧式三軸試験機 / 粉砕 / ラプチャー / ガス圧式三軸圧縮試験 |
|---|
| Research Abstract |
In order to clarify the mechanism of rock pulverization around fault, a series of stick-slip experiment was conducted with a gas-medium triaxial apparatus, recording strains with5MHz sampling rate for up to10 channels. The mechanical data confirmed a supershear velocity of the propagation of rapture front during large stick-slip. Fracture pattern in the pulverized cores shows obvious dependence on the slip direction. It is likely that anomalously high axial stress caused strong tension stress on the slip plane during slip resulted in pervasive mode I fractures.
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