概括
地震波揭示了塞拉内华达山脉下方的高速岩层,可能是一个古老的ophiolite板. 这一层解释了来自内华达州试验场的更快的波浪旅行时间,表明塞拉根深入地幔.
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:
- 整个内华达山脉的地震波传播显示出方向异常.
- 一个无法解释的观察是,地震波从内华达州的试验场到达的速度更快.
研究的目的:
- 为了调查异常地震波穿越塞拉内华达山脉的旅行时间的原因.
- 为了确定塞拉内华达山脉的深层结构.
主要方法:
- 分析来自各种来源,包括地震和爆炸的地震波旅行时间.
- 地质物理建模用于解释地震数据并推断地下结构.
主要成果:
- 地震波从所有方向都会延迟到达,除了内华达州的试验场外.
- 来自内华达州试验场的早期到达波浪表明,它通过高速岩层出现.
- 这个高速的层被假设为一个起的ophiolite板.
- 塞拉斯山脉的根延伸到大约55公里的地幔深处.
结论:
- 一个起的ophiolite板块可能会在内华达山脉下面形成一个高速的层.
- 塞拉内华达山脉的深层结构包括一个根源,延伸到地幔.
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