内层地震:卡斯卡迪亚板块的脱水
Leiph A Preston1, Kenneth C Creager, Robert S Crosson
1Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195, USA. preston@ess.washington.edu
概括
研究人员绘制了华盛顿Juan de Fuca板块的3D地震结构. 这揭示了两种不同的地震起源:地幔中的蛇形石脱水和地中的玄武岩转化为生态石.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 构造学 构造学 构造学 构造学
背景情况:
- 胡安·德·福卡板块在北美底下沉积,产生复杂的地震活动.
- 了解引板的结构是解读地震机制的关键.
研究的目的:
- 为了确定三维压缩波速度结构和反射器几何形状的潜伏的胡安·德·福卡板.
- 为了调查在卡斯卡迪亚俯冲区内星系内地震的起源.
主要方法:
- 同时逆转折射和广角反射的地震波的行程时间.
- 3D地震速度建模和地震转移.
主要成果:
- 确定了岩板的地-地幔边界 (Moho).
- 根据它们与莫霍相对的位置,将内部地震分为两个不同的组.
- 在45公里深的莫霍海底上方的地震发生在沉降的海洋地幔中; 下方的地震发生在沉降的地中.
结论:
- 在实验室内发生的上下地震与蛇形石脱水有关.
- 在实验室内下沉的地震归因于玄武岩到生态石的转变.
- 为了解卡斯卡迪亚潜水带的地震发生提供了一个新的框架.
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