由于粉末滑,故障减弱和地震不稳定
Ze'ev Reches1, David A Lockner
1School of Geology and Geophysics, University of Oklahoma, 100 East Boyd Street, Norman, Oklahoma, USA. reches@ou.edu
Nature
|September 25, 2010
概括
新形成的断层作为滑剂,在地震期间显著削弱断层. 在花岩实验中观察到的这种动态减弱机制解释了地震的不稳定性和地球上的断层行为.
科学领域:
- 地质物理学 地质物理学
- 地震物理学 地震物理学
- 岩石机械学 岩石机械学
背景情况:
- 地震不稳定与加速滑动期间断层减弱有关.
- 驱动这种减弱的精确机制,尽管进行了广泛的研究,但仍然在很大程度上无法解释.
研究的目的:
- 为了研究在地震滑动率下切割的实验断层中的动态削弱机制.
- 为了确定新形成的断层口在地震不稳定性中的作用.
主要方法:
- 切割房间干燥,固体花岩块以模拟故障行为.
- 由于细粒度岩石粉末 (形) 形成而导致断裂强度降低的分析.
- 随着时间的推移,观察的老化和断裂强度的恢复.
主要成果:
- 在10-60毫米/秒的滑动速度下,新形成的隙组织成一个薄薄的变形层.
- 这种动态层将断层强度降低了2-3的因素.
- 断层恢复了它的力量,因为洞穴在滑动后变老了.
结论:
- 动态沟形成是脆弱地中地震不稳定的关键机制.
- 新形成的孔作为滑剂,解释了观测到的地震特性.
- 这种机制适用于各种故障条件,组成和温度.
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