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P波和S波接收函数的贝叶斯联合反演

DOI: 10.6038/cjg20130108, PP. 69-78

Keywords: P波和S波接收函数,联合反演,贝叶斯理论,岩石圈结构

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Abstract:

S波接收函数对于研究岩石圈速度结构具有重要价值.本文利用合成地震图技术研究了S波接收函数的动力学特征.在接收函数非线性复谱比反演方法的基础上,发展了基于贝叶斯理论的P波和S波接收函数的非线性联合反演方法.结果表明:(1)适用于S波接收函数反演的震中距范围约为55°~80°,S波接收函数反演要求所用远震事件的震级大于5级;(2)与陡变的岩石圈底部界面(LAB)相比,梯度带类型LAB上生成的SLP转换波相对较弱,台站下方的沉积盖层有助于相对增强SLP震相;(3)由于S波接收函数径向分量不符合δ脉冲,不依赖于等效震源假定的三分量接收函数多道最大或然性反褶积方法更适合S波接收函数的估计;(4)数值检验的结果表明,在初始模型速度参数偏离真实模型20%的情况下,本文的方法能够预测300km深度范围内的P波和S波速度结构;(5)观测数据的反演结果表明,由于P波接收函数低频分量相对不足,本文的联合反演方法对于大于100km深度上地幔的S波速度结构约束相对较弱.

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