下层地的地震引起的变化
Bjørn Jamtveit1, Yehuda Ben-Zion2, François Renard3,4
1Physics of Geological Processes (PGP), The Njord Centre, Department of Geosciences, University of Oslo, Oslo, Norway. bjorn.jamtveit@geo.uio.no.
Nature
|April 27, 2018
概括
在地下部发生的地震会引发流体透, 这种地震活动影响了整个地的地力学.
科学领域:
- 地质学
- 构造学
- 石油学
背景情况:
- 低地的结构和变态进化影响了土壤形成,影响了沉积盆地,山根和高地形地区.
- 在产卵前,下层通常是干燥的,不透的,机械坚固的.
- 在生过程中,沿剪切区域的液体透控制了下层地的演变.
研究的目的:
- 研究下层地地震及其余震在驱动流体透和随后的变形/结构转变中的作用.
- 了解地震活动对地地力学的"自上而下的"影响.
主要方法:
- 在挪威西部的贝尔根弧度,从下层地地震开始的断层剪切区域的分析.
- 研究地震滑动,压力脉冲和下层的余震产生之间的关系.
- 在地震事件后检查流体驱动的变形和结构变化.
主要成果:
- 低地的地震会产生压力脉冲,引发大量的余震活动.
- 流体透是由这些余震驱动的,导致下层地发生显著的变形和结构变化.
- 这项研究证明了地地力学上的"自上而下"效应,将短期地震过程与长期构造进化联系起来.
结论:
- 下层地的地震活动是流体运输和地变化的关键机制.
- 地震引起的余震在修改地下层的机械特性和结构方面起着至关重要的作用.
- 这项研究将过程连接到截然不同的时间尺度,
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