概括
在1986年北棕泉地震之后观察到地震磁偏移. 这些永久磁场变化为难以捉摸的地震磁效应提供了第一个直接证据.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 地磁主义 地磁主义
背景情况:
- 圣安德烈亚斯断层由磁力计阵列监测,以检测地震磁效应.
- 地震磁场效应,或地震引起的磁场变化,早已被预期,但很少被观察到.
研究的目的:
- 报告第一次对地震磁偏移的直接观测.
- 分析观察到的地震磁偏移的特征,并将其与地震模型进行比较.
主要方法:
- 利用在圣安德烈亚斯断层沿线运行的24个质子磁力计的差异连接阵列.
- 1986年北棕泉地震前后记录的磁场数据.
主要成果:
- 在3公里和9公里中心距离分别观测到1.2和0.3纳米斯拉的地震磁偏移.
- 观察到的偏移与地震磁模型一致,其中包括在班宁断层上的20厘米右侧破裂.
- 观察到的磁性变化是永久性的,并在20分钟内完成.
结论:
- 这项研究提供了地震磁效应的第一个直接证据.
- 这些数据支持地震引起的磁场变化的物理模型.
- 电动效应不太可能解释观察到的永久磁场变化.
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Magnetic field lines follow several hard-and-fast rules:
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