概括
1983年的科林加地震弹性地折叠了地层,而不是破裂了地表. 对地震,地质测量和地质数据的分析揭示了地下断层滑动率和地震复发间隔.
科学领域:
- * 地震学和构造学
背景情况:
- * 1983年科林加地震 (Mw 6.5) 并没有破裂表面沉积物.
- * 相反,它导致了上层地的弹性折叠.
研究的目的:
- * 为了估计地下断层滑动率.
- * 为了确定Coalinga地区的地震重复时间.
- * 调查隐藏的反向断层与活跃折叠之间的关系.
主要方法:
- * 集成地震数据.
- * 利用地质测量测量.
- *对地质证据的分析.
主要成果:
- *地震导致浅层地的弹性折叠.
- *估计了地下断层滑动率和地震复发间隔.
- *在过去20年中,三次较大的地震 (高达7.5MW) 发生在活跃折叠下面的盲目反向断层上.
结论:
- *地震可能发生在隐藏在表面折叠下的断层上.
- *弹性地变形在地震事件中起着重要作用.
- *了解盲断层对于地震危险评估至关重要.
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