在圣安德烈亚斯断层深处发生非火山性震动
Robert M Nadeau1, David Dolenc
1Berkeley Seismological Laboratory, 211 McCone Hall, University of California, Berkeley, CA 94720-4760, USA. nadeau@seismo.berkeley.edu
概括
科学家们在加利福尼亚州圣安德烈亚斯断层深处发现了非火山震动活动. 这种发生在地震产生的区域以下的地震信号可能与当地地震模式相关.
科学领域:
- *地震学和构造物理学:研究地震现象和板块边界动态.
背景情况:
- *圣安德烈亚斯断层是加利福尼亚州的一个主要的变形板边界,与1857年特吉安堡地震等重大地震事件有关.
- *地震活动,包括地震,主要被认为起源于地球地的地震带.
研究的目的:
- * 识别和描述圣安德烈亚斯断层沿线的非火山震动活动.
- * 确定这次地震的深度和潜在关系与当地的地震性.
主要方法:
- *对地震数据的分析,以检测长时间的地震信号,缺乏明确的P或S波 (非火山震动).
- * 在转变板边界区域内地理定位震动活动.
主要成果:
- * 在20至40公里深处发现非火山震动活动.
- * 这次地震发生在典型的地震带 (上方15公里) 以下.
- *观察到震动活动率与当地地震活动变化之间的潜在相关性.
结论:
- * 在圣安德烈亚斯断层深处,地震带以下,存在非火山性震动.
- *这种深度地震活动可能在断层系统的更广泛的地震行为中发挥作用.
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