在Coso的山脊余震被热解压制
Kyungjae Im1, Jean-Philippe Avouac2, Elías R Heimisson2,3
1Geology and Planetary Science Division, California Institute of Technology, Pasadena, CA, USA. kjim@caltech.edu.
Nature
|July 1, 2021
概括
在Coso的地热生产削减了断层应力,防止Ridgecrest地震的余震. 这种减压也改变了断层风格,并可能阻碍大地震的传播.
科学领域:
- 地质学
- 地震学
- 地热能源
背景情况:
- 地热和火山地区容易引发地震.
- 科索地热场位于2019年里奇克雷斯特地震的表面裂附近.
- 尽管有预期的压力变化,但在Coso领域没有观察到余震.
研究的目的:
- 调查科索地热场为什么没有经历里奇克雷斯特地震的余震.
- 了解地热发电对当地地震和压力积累的影响.
主要方法:
- 分析来自科索地热场的地震数据.
- 由于热量产生而导致地热水库内的应力变化的建模.
- 在里奇克雷斯特地震发生之前和之后的压力条件的比较.
主要成果:
- 在Coso的30年地热产量显著减少了水库内的剪切应力.
- 热收缩最初导致地震,但后来减少了对余震的应力.
- 减压改变了断层的风格并抑制了余震的触发.
结论:
- 地热能源的提取可以导致水库的压力显著减少.
- 这种压力消耗可以防止地震余震并改变断层的行为.
- 减压区域可能会阻碍大型地震事件的传播.
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