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中国陆区S波分裂与上地幔地震各向异性
引用本文:刘堃,张中杰,滕吉文,孙克忠,胡家富.中国陆区S波分裂与上地幔地震各向异性[J].地球物理学进展,2001,16(2).
作者姓名:刘堃  张中杰  滕吉文  孙克忠  胡家富
基金项目:国家自然科学基金,国家自然科学基金
摘    要:本文利用中国大陆区共8个台站所观测到地震事件的S波数据,采用相关分析的手段以及对观测数据重建的技术,进行了S波分裂参数—快慢波延迟时间与快波偏振方向的计算,并分析了S波分裂参数与中国陆区上地幔物质运动的相互关系.研究结果表明:兰州台下的S波分裂时差最小,北京台下的最大.中国东部地区上地幔运动方向以西北向为主,西部地区以北偏西为优势.

关 键 词:天然地震台网资料  S波分裂  上地幔  地震各向异性

S-WAVE SPLITTING AND SEISMIC ANISOTROPY OF UPPER-MANTLE IN CHINA MAINLAND
LIU Kun,Zhang Zhong-jie,TENG Ji-Wen,SUN Ke-zhong,HU Jia-fu.S-WAVE SPLITTING AND SEISMIC ANISOTROPY OF UPPER-MANTLE IN CHINA MAINLAND[J].Progress in Geophysics,2001,16(2).
Authors:LIU Kun  Zhang Zhong-jie  TENG Ji-Wen  SUN Ke-zhong  HU Jia-fu
Abstract:We applied the methods of correlation and reconstruction to the S-wave data observed at 8 stations in China mainland and calculated the delay time and fast polarization of the S-wave splitting. The relationship between the splitting parameters and the substance movement in upper-mantle of China mainland has been analyzed. The results show that, the smallest delay time of S-wave splitting occurs at the station of LZH (Lanzhou), and the biggest occurs at the station of BJI (Beijing); The movement of upper-mantle in Eastern China is mainly north-westward, and westward from north in Western China.
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