从壳幔地震各向异性初探华北地区壳幔耦合关系
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摘要
根据首都圈地震台网、国家地震台网、IRIS台站资料,并比较了流动的华北地震台阵部分台站资料的结果,利用地震各向异性分析,得到减少局部构造影响后的华北地区(至少是华北地区北部)的地壳背景水平主压应力方向为北东95.1°±15.4°,穿透壳幔的SKS分裂的快剪切波偏振平均值为北东110.2°±15.8°.而台站分析也显示,地壳内近场资料的快剪切波偏振与SKS快剪切波偏振总是相差十几度以上.不同周期下的Rayleigh面波相速度方位各向异性快波优势方向也同样揭示出随深度增加快波优势方向的变化.这个特征暗示华北地区的壳幔耦合关系可能既不是简单的壳幔解耦型,也不是壳幔强耦合型,可能是两种模式共存的不均匀分布,或者是物理性质介于两者之间的渐变模式.研究表明,在分析穿透整个岩石圈的SKS分裂和地表的GPS观测的基础上,增加揭示地壳各向异性的近场资料剪切波分裂,结合面波的方位各向异性,可以更准确地多方位刻画壳幔各向异性性质,进而探讨壳幔的耦合关系.
引文
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