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南海及邻区地壳上地幔三维S波速度结构的面波波形反演>.
引用本文:曹小林,朱介寿,赵连锋,曹家敏,洪学海.南海及邻区地壳上地幔三维S波速度结构的面波波形反演>.[J].地震学报,2001,23(2):113-124.
作者姓名:曹小林  朱介寿  赵连锋  曹家敏  洪学海
作者单位:1)中国长沙410073国防科技大学计算机学院 2)中国成都610059成都理工学院信息工程与地球物理系
基金项目:国家自然科学基金!重点项目 ( 4973 4 1 50 ),国家高性能计算基金资助
摘    要:对南海及邻区中国数字地震台网4个台站接收到的328条长周期地震记录的面波波形进行分块波形反演.分块波形反演把大尺度的优化问题转化为小尺度的优化问题,采用非线性优化方法求解,从而得到南海及邻区22网格划分、从地表深至430km 的地壳上地幔三维S波速度结构,并用检验板法进行了分辨率分析.结果表明,海域、岛弧和大陆在速度分布、岩石圈和软流圈存在明显的结构差异. 

关 键 词:南海及邻区  面波波形  分块波形反演  三维S波速度结构
文章编号:0253-3782(2001)02-0113-12
修稿时间:1999年12月21

THREE DIMENSIONAL SHEAR WAVE VELOCITY STRUCTURE OF CRUST AND UPPER MANTLE IN SOUTH CHINA SEA AND ITS ADJACENT REGIONS BY SURFACE WAVEFORM INVERSION
Cao Xiaolin,Zhu Jieshou,Zhao Lianfeng,Cao Jiamin,Hong Xuehai.THREE DIMENSIONAL SHEAR WAVE VELOCITY STRUCTURE OF CRUST AND UPPER MANTLE IN SOUTH CHINA SEA AND ITS ADJACENT REGIONS BY SURFACE WAVEFORM INVERSION[J].Acta Seismologica Sinica,2001,23(2):113-124.
Authors:Cao Xiaolin  Zhu Jieshou  Zhao Lianfeng  Cao Jiamin  Hong Xuehai
Abstract:We assembled approximately 328 seismic records. The data set was from 4 digitally recording long-period and broadband stations of CDSN. We carried out the inversion based on the partitioned waveform inversion (PWI). It partitions the large-scale optimization problem into a number of independent small-scale problems. We adopted surface waveform inversion with an equal block (2°×2°) discretization in order to acquire the images of shear velocity structure at different depths (from surface to 430 km) in the crust and upper-mantle. The resolution of all these anomalies has been established with “check-board” sensitivity tests. These results show significant difference in velocity, lithosphere and asthenosphere structure between South China Sea and its adjacent regions.
Keywords:South China Sea and its adjacent regions  surface waveform  partitioned waveform inversion  three dimensional shear wave velocity structure
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