在台湾的Chelungpu断层区域的钻井阵列中观测到的同otropic事件
Kuo-Fong Ma1, Yen-Yu Lin, Shiann-Jong Lee
1Department of Earth Sciences, and Institute of Geophysics, National Central University, Taiwan, Republic of China. fong@ncu.edu.tw
概括
研究人员观察到台湾的地震事件.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 岩石力学 岩石力学 岩石力学
背景情况:
- 剪切故障主导了断层区域的地震过程.
- 高流体压力可以诱导岩石破裂,但在断层区域缺乏直接观察.
研究的目的:
- 为了研究在断层区域中可能由高流体压力引起的地震事件.
- 了解地震活跃地区自然水力压裂的机制.
主要方法:
- 来自台湾切隆普断层区域的钻井阵列地震数据的分析.
- 地震事件源机制的建模.
主要成果:
- 在主要滑动区下方的富含流体区域观察到小地震事件 (I型).
- 模拟事件具有同位素的,非切割源机制.
- 将事件解释为可能代表自然液压断裂的事件.
结论:
- 提供了在断层区域中流体压力诱导的岩石断裂的直接观察.
- 与自然液压断裂和流体特征形成有关的地震事件.
- 建议这些自然过程与人工液压压裂之间的相似性.
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