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川滇地区壳幔地震各向异性研究进展
引用本文:张艺,高原,赵镇岭.川滇地区壳幔地震各向异性研究进展[J].中国地震,2018,34(2):207-218.
作者姓名:张艺  高原  赵镇岭
作者单位:上海市地震局;中国地震局地震预测研究所(地震预测重点实验室)
基金项目:国家重点研发计划课题(2016YFC0600302)、国家自然科学基金项目(41474032)及上海市科委社发领域科研项目“短临地震地电观测新技术研究”(16dz1206000)共同资助
摘    要:根据川滇地区已有的地震各向异性研究结果,利用体波、面波资料的结果,分析川滇地区不同构造尺度、不同深度的地震各向异性特征。对比不同方法研究川滇地区介质各向异性的特点,探讨了该地区的介质连续性及壳幔耦合状态。分析认为,地壳上地幔各向异性的差异表明,川滇地区具有复杂的地壳及上地幔形变机制。因此,对于川滇地区壳幔地震各向异性的深入理解,需在理论上和高密度数据资料基础上加强量化分析和综合研究。

关 键 词:川滇地区  地震各向异性  S波分裂  体波  面波  地壳  上地幔
收稿时间:2017/3/4 0:00:00
修稿时间:2017/6/1 0:00:00

Reviews on the Seismic Anisotropy in the Crust and Mantle of Sichuan-Yunnan Area,China
Zhang Yi,Gao Yuan and Zhao Zhenling.Reviews on the Seismic Anisotropy in the Crust and Mantle of Sichuan-Yunnan Area,China[J].Earthquake Research in China,2018,34(2):207-218.
Authors:Zhang Yi  Gao Yuan and Zhao Zhenling
Institution:Shanghai Earthquake Agency, Shanghai 200062, China,Key Laboratory of Earthquake Prediction, Institute of Earthquake Forecasting, CEA, Beijing 100036, China and Shanghai Earthquake Agency, Shanghai 200062, China
Abstract:The seismic anisotropy characteristics of different tectonic scales and different depths are summarized through the analysis of body wave and surface wave data based on the existing seismic anisotropy results in the Sichuan-Yunnan area. We introduce the characteristics of medium anisotropy by comparing different methods. Then we analyze the continuity and coupling of crust and mantle. The difference of the seismic anisotropy between the crust and mantle can indicate various deformation mechanisms. Therefore,we propose that the seismic anisotropy in the crust and mantle of the Sichuan-Yunnan area should be studied more quantitatively and synthetically both in theory and high density data process.
Keywords:Sichuan-Yunnan area  Seismic anisotropy  Shear-wave splitting  Body wave  Surface wave  Crust  Upper mantle
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