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在地幔最底层的佩洛夫斯基特后发生的反相关的地震速度异常
Alexander R Hutko1, Thorne Lay, Justin Revenaugh
1Earth and Planetary Sciences Department, University of California, Santa Cruz, CA 95064, USA.
地震波揭示了地球深层地幔的明显变化. 速度表明在核心-地幔边界附近的矿物阶段过渡,影响地震波的行为.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 矿物物理 矿物物理
背景情况:
- 地球深层地幔表现出复杂的热,化学和矿物质特性.
- 精确的地震学表征对于理解这些地球深层结构至关重要.
- 核心-地幔边界区域以显著的异质性而闻名.
研究的目的:
- 在地震学上描述地球最下层地幔的结构.
- 为了研究核-地幔边界附近的地震波速异常.
- 了解矿物阶段过渡对地震性能的影响.
主要方法:
- 分析了超过10,000个穿过深层地幔的P和S地震波.
- 应用堆叠,迁移和建模技术.
- 在Cocos板下方的核心-地幔边界以上的结构的分辨率.
主要成果:
- 观察到P波速度 (Vp) 减少了-0.07%,S波速度 (Vs) 在~2570公里深处增加了1.5%.
- 在相同深度检测到批量声速 (Vb) 降低了-1.0%.
- 发现Vb和Vs异常之间存在局部反相关性,与矿物学变化一致.
结论:
- 观察到的地震异常可以通过酸矿转变为后矿来解释.
- 这种过渡显著增加了剪切模块,同时对散装模块的影响很小.
- 地震数据提供了深层地幔矿物质复杂性和相变的证据.
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