概括
岩石应力变化改变了磁性特性,可能预测地震. 一个磁力计阵列检测到在圣安德烈亚斯断层爬行之前的地磁场转移,表明压磁信号可能预测断层活动.
科学领域:
- 地质物理学 地质物理学
- 地球科学 地球科学 地球科学
- 地震学 地震学
背景情况:
- 岩石表现出压磁性质,这意味着应力变化会影响其磁性易感性和残留磁化.
- 这些磁力变化可以影响当地的地磁场,为监测地下压力提供了潜在的方法.
研究的目的:
- 为了研究与活性断层应力相关的压磁信号.
- 为了确定地磁场的变化是否可以在断层活动之前发生.
主要方法:
- 一个微分阵列的磁力计自1965年以来一直在运行.
- 该阵列位于圣安德烈亚斯断层,用于在活跃应力条件下检测压磁效应.
主要成果:
- 在加利福尼亚州霍利斯特附近观察到当地地磁场变化.
- 这些磁场变化发生在圣安德烈亚斯断层突然爬行移位事件发生前几十个小时.
结论:
- 观察到的地磁场变化表明可以检测到压磁信号.
- 压磁监测可能提供一种预测活性断层应力和随后的爬行事件的手段.
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