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云南地区地壳中上部横波速度结构研究
引用本文:何正勤,叶太兰,苏伟.云南地区地壳中上部横波速度结构研究[J].地球物理学报,2004,47(5):838-844.
作者姓名:何正勤  叶太兰  苏伟
作者单位:中国地震局地球物理研究所,北京 100081
基金项目:地震科学联合基金项目 ( 10 10 86),中国地震局重点项目 (中国大陆数字壳幔结构 )
摘    要:根据云南地区的基阶瑞利波相速度频散资料,用面波层析成像方法反演得到该区域中上地壳S波速度结构. 给出了研究区域内在4个深度上的S波速度水平分布图像和沿100.5°E、24°N、25°N、26°N及27°N的S波速度-深度剖面图. 结果表明:在小江断裂与红河断裂围成的川滇菱形块体内,26~30km深度处的速度明显低于周边地区,其南段从地表到15km深度均为明显的低速区域. 云南地区的强震(M>6.0)震中位置与S波速度分布图像具有明显的相关性,主要分布于高速与低速的过渡区域.

关 键 词:瑞利波相速度  层析成像  S波速度结构  云南地区  
文章编号:0001-5733(2004)05-0838-07
收稿时间:2003-11-4
修稿时间:2004-6-14

S-WAVE VELOCITY STRUCTURE OF THE MIDDLE AND UPPER CRUST IN THE YUNNAN REGION
HE Zheng-Qin YE Tai-Lan SU Wei Institute of Geophysics,China Earthquake Administration,Beijing ,China.S-WAVE VELOCITY STRUCTURE OF THE MIDDLE AND UPPER CRUST IN THE YUNNAN REGION[J].Chinese Journal of Geophysics,2004,47(5):838-844.
Authors:HE Zheng-Qin YE Tai-Lan SU Wei Institute of Geophysics  China Earthquake Administration  Beijing  China
Institution:Institute of Geophysics, China Earthquake Administration, Beijing 100081, China
Abstract:The dispersion data of phase velocities of the fundamental mode Rayleigh wave are used in this paper, the S wave velocity structure of the middle and upper crust in Yunnan region is inverted. The horizontal distribution maps of S wave velocities at four depths and S wave velocities on profiles along 24°N, 25°N, 26°N, 27°N and 100.5°E in the study region are given. The results show that within the range of 26~30km depth, the S wave velocity in the Sichuan Yunnan rhombic block is obviously lower than that in surrounding areas; In the south rhombic block, there is a low velocity region to exist in the range from ground surface to 15km depth. The epicentral locations of strong earthquakes with M>6.0 in Yunnan region are closely related to the S wave velocity distribution. They are mainly distributed in zones of transition between low and high velocities.
Keywords:Phase velocity of Rayleigh waves  Tomographic imaging  S-wave velocity structure  Yunnan region  
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