地震异质性:在地幔中追踪板块动态
1Department of Geology and Geophysics, Yale University, Post Office Box 208109, New Haven, CT 06520-8109, USA.
概括
弹性异构,即地震波的速度因方向而异,是理解地球地幔和地的关键. 这种由矿物方向驱动的现象有助于地球物理学家探索岩石纹理和地幔动态.
科学领域:
- 地质学和地球科学 地球物理学和地球科学
- 地震学 地震学
- 矿物物理 矿物物理
背景情况:
- 当地震波速度取决于方向时,弹性异构性发生.
- 在地球的地幔和地中,由于方向流或变形,导向矿物质会诱导弹性异质性.
- 地震产生压缩 (P) 和剪切 (S) 波,这些波在异型岩石中相互作用.
研究的目的:
- 阐明地震波行为在异构介质中的作用.
- 突出地质物理学家如何利用这些现象来研究地球的结构和动态.
- 在理解地质过程中展示地震异性质的应用.
主要方法:
- 在异型岩石中对地震波传播 (P和S波) 的分析.
- 观测地震波的合,散射和双断.
- 解释在异质环境中产生的混合波极化.
主要成果:
- 在异型岩石中,地震波的合会导致诸如散射和双折射等复杂的行为.
- 这些复杂的波浪行为产生波浪与混合极化.
- 对这些现象的研究提供了对地下物质性质的洞察.
结论:
- 弹性异构是解释来自地球内部的地震数据的关键因素.
- 地质物理地幔和地岩层结构的探索依赖于理解地震异性质.
- 地震异构分析有助于绘制地幔对流和重建构造物历史.
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