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汶川地震断裂带科学深钻附近上地壳S波分裂特征
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摘要
<正>地壳介质中遍布大量定向排列的EDA(extensive-dilatancy anisotropy,张性扩容各向异性)微裂隙(Crampin,et al.,1985),在区域主压应力的作用下,地壳岩石中裂隙的定向排列形成了地震各向异性。S波在各向异性介质中传播时,对地壳介质应力场的变化十分敏感,会分裂成一对接近垂直且速度不同的快、慢波,通过S波快波的优势偏振方向可以获得区域内主压应力的方向,从而揭示地壳介质的各向异性特征(Silver,et al.,1991)。S波快波偏振的优势方向与台站下方的水平主压应力方向一
引文
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