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地震 ›› 2008, Vol. 28 ›› Issue (2): 65-73.

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地壳介质剪切波分裂研究的部分进展

太龄雪, 高原   

  1. 中国地震局地震预测研究所, 北京 100036
  • 收稿日期:2007-09-17 修回日期:2007-11-12 出版日期:2008-04-30 发布日期:2021-10-29
  • 作者简介:太龄雪(1982), 女, 吉林延吉人, 2005年在读研究生, 主要从事数字地震学等研究。
  • 基金资助:
    中国地震局地震预测研究所基本科研专项(2007-13); 地震行业科研专项(200708008)

Some progresses of shear-wavesplitting in the crust

TAI Ling-xue, GAO Yuan   

  1. Institute of Earthquake Science, CEA, Beijing 100036
  • Received:2007-09-17 Revised:2007-11-12 Online:2008-04-30 Published:2021-10-29

摘要: 剪切波穿过各向异性介质传播时会发生分裂现象, 而在地壳中产生各向异性的主要因素是大量充满液体的定向排列的微裂隙。 通过剪切波分裂参数可以研究地壳介质的特性、 地壳应力状态及应力场的变化, 并可用于地震预测。 利用地壳介质各向异性特征研究断层性质也是一个新的动向。

关键词: 剪切波分裂, 各向异性, 地壳, 偏振, 时间延迟, 应力

Abstract: Seismic shear waves split when traveling through anisotropic media, and the anisotropy in the crust is mainly the result of stress-aligned fluid-saturated grain-boundary cracks. Analysis of anisotropy-induced shear wave splitting is used for studying the feature of crustal media, the condition and variation of crustal stress, and earthquake forecast as well. It is also a new attempt to study the nature of faults by means of analysis of anisotropy in crust.

Key words: Shear-wave splitting, Anisotropy, Crust, Polarization, Time-delay, Stress

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