用小波变换方法反演接收函数  

INVERSION OF RECEIVER FUNCTION BY WAVELET TRANSFORMATION

作　　者：吴庆举[1] 田小波[1] 张乃铃[1] 李桂银[1] 曾融生[1] 

机构地区：[1]中国地震局地球物理研究所,中国北京100081

出　　处：《地震学报》2003年第6期601-607,共7页Acta Seismologica Sinica

基　　金：国家自然科学基金项目 ( 4 9974 0 2 1)资助

摘　　要：提出了一种用小波变换方法反演接收函数的新方法 .通过对接收函数作离散小波变换 ,将接收函数展开到不同分辨尺度 ,从一给定的初始模型出发 ,分别在不同分辨尺度上用广义线性反演方法 ,对展开后的接收函数进行反演 .并将低阶接收函数的反演结果作为高阶接收函数的初始模型 ,在大尺度空间找到包含全局极小值的一个邻域 ,并逐步缩小该邻域 .渐进地获取介质结构的跳变信息 ,从而保证反演结果稳定地收敛到全局极小点 ,降低接收函数波形反演对初始模型的依赖 ,尽可能克服波形反演的非唯一性 。A new method for receiver function inversion by wavelet transformation is presented in this paper. Receiver func-tion is expanded to different scales with different resolution by wavelet transformation. After an initial model be-ing taken, a generalized least-squares inversion procedure is gradually carried out for receiver function from low to high scale, with the inversion result for low order receiver function as the initial model for high order. A neighborhood containing the global minimum is firstly searched from low scale receiver function, and will gradu-ally focus at the global minimum by introducing high scale information of receiver function. With the gradual ad-dition of high wave-number to smooth background velocity structure, wavelet transformation can keep the inver-sion result converge to the global minimum, reduce to certain extent the dependence of inversion result on the initial model, overcome the nonuniqueness of generalized least-squares inversion, and obtain reliable crustal and upper mantle velocity with high resolution.

关 键 词：小波变换 反演 接收函数 波形反演 

分 类 号：P315.31[天文地球—地震学]