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接收函数近邻反演方法的改进和对海拉尔台下地壳速度结构的研究

  • 沈旭章 ,
  • 周蕙兰
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  • 中国科学院研究生院计算地球动力学重点实验室, 北京 100049

收稿日期: 2004-07-28

  修回日期: 2004-11-25

  网络出版日期: 2005-05-15

基金资助

国家自然科学基金(40374009)资助

Improvement on Inversion Method of Neighborhood Algorithm with Receiver Functions and Research of Crust Structure under Station HLR

  • SHEN Xu-Zhang ,
  • ZHOU Hui-Lan
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  • Laboratory of Computational Geodynamics, Graduate School of the Chinese Academy of Sciences, Beijing 100049, China

Received date: 2004-07-28

  Revised date: 2004-11-25

  Online published: 2005-05-15

摘要

数值试验结果指出,用接收函数反演地壳速度结构时,在正演和反演过程中使用不匹配的地壳模型参数化方式,将对结果产生不良影响;同时发现,在处理实际资料时将接收函数归一化,可能会丢弃介质信息.在此基础上,改进了接收函数和近邻算法反演地壳速度结构的程序,并用来反演了海拉尔台下的地壳速度结构.

本文引用格式

沈旭章 , 周蕙兰 . 接收函数近邻反演方法的改进和对海拉尔台下地壳速度结构的研究[J]. 中国科学院大学学报, 2005 , 22(3) : 322 -328 . DOI: 10.7523/j.issn.2095-6134.2005.3.010

Abstract

The numerical test shows that the ill effect will be brought in the inversion result of velocity structure with receiver functions when the parameterized models in the forwarding and inversing procedures are not matched. Some information will be lost in the real data processing when the observed and synthetic receiver functions are normalized respectively.Accordingly, the inversion program of Neighborhood Algorithm with receiver functions is improved and then the crust velocity structure under station HLR is obtained in this paper.

参考文献

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