断层粗度控制了注射诱导的地震性.
Lei Wang1, Grzegorz Kwiatek1, François Renard2,3,4
1Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Geomechanics and Scientific Drilling, Potsdam 14473, Germany.
概括
断层粗度通过定位地震事件并改变它们的特征,显著影响流体诱导的地震性. 了解这些影响对于预测液体注射操作期间可能发生的失控事件至关重要.
科学领域:
- 地质物理学 地质物理学
- 地震科学 地震科学 地震科学
- 岩石机械学 岩石机械学
背景情况:
- 表面粗在自然断层中很常见,影响了构造地震的动态.
- 断层粗度对流体诱导的地震性的影响尚不清楚.
研究的目的:
- 研究断层几何和应力异质性如何影响流体诱导的断层滑动.
- 分析与在粗与光滑断层中注射液体相关的地震性特征.
主要方法:
- 在带有光滑和粗断层的砂岩样本上进行实验室液体注射实验.
- 数字建模来补充实验发现.
主要成果:
- 与光滑断层相比,粗断层表现出较慢的滑动,降低的滑动速度和较低的滑动减弱率.
- 断层粗度和应力异质性控制低中心分布,频率-大小关系,以及诱导声学排放 (AE) 的源机制.
- 粗断层上的AE在压力度周围的空间局部化,显示非双机制和较低的古登伯格-里赫特b值.
结论:
- 断层粗度会影响流体诱导的地震性的空间分布和特征.
- 监测诱导的微地震性可以帮助识别地震活动的本地化和预测危险事件.
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