基于密集台阵资料的S波分裂研究云南宾川上地壳各向异性特征  

Analyzing the characteristics of the upper crustal anisotropy in Binchuan,Yunnan Province based on dense arrays and shear wave splitting

作　　者：豆辉 王宝善[1,2] 徐逸鹤 王伟涛[1] 张博[1] DOU Hui;WANG BaoShan;XU YiHe;WANG WeiTao;ZHANG Bo(Institute of Geophysics,China Earthquake Administration,Beijing 100081,China;School of Earth and Space Science,University of Science and Technology of China,Hefei 230026,China;Department of Earth Sciences,University of Cambridge,Cambridge CB30EZ,United Kingdom;Geophysics Section,School of Cosmic Physics,Dublin Institute for Advanced Studies,Dublin D02Y006,Ireland)

机构地区：[1]中国地震局地球物理研究所,北京100081 [2]中国科学技术大学地球和空间科学学院,合肥230026 [3]英国剑桥大学地球科学系,剑桥CB30EZ [4]爱尔兰都柏林高等研究院宇宙物理学学院地球物理学分部,都柏林D02Y006

出　　处：《地球物理学报》2021年第12期4292-4307,共16页Chinese Journal of Geophysics

基　　金：国家自然科学基金(41904084,41790462,41790463和41804054)联合资助.

摘　　要：上地壳地震各向异性主要受区域应力引起的裂隙定向排列影响,也受局部构造单元,如断裂带等的影响.受地震台阵台间距的限制,系统性地研究断裂带等构造因素对各向异性影响的研究还较少.基于云南宾川地区密集台阵在两个月内记录到的9819个S波记录,我们使用MFAST(Multiple Filter Automatic Splitting Technique)方法获得了831个高质量的横波分裂结果.结果显示,(1)该区域内的平均快波偏振方向为NNW向,与区域最大水平主压应力方向一致;(2)空间分布上,断裂带附近台站的快波偏振方向呈现与断裂带走向相关的特征;(3)平均慢波时延为0.087±0.002 s,计算得到的各向异性强度为2.4%,高于云南地区的平均值.研究结果表明,宾川地区的上地壳各向异性主要受区域应力控制,局部特征受断裂带的改造作用,各向异性强度较强.本研究展示了密集台阵在系统性地研究上地壳各向异性的优势,即利用高密度的空间采样可以更好地分析上地壳各向异性的空间分布细节和影响机制.Seismic anisotropy in the upper crust is mainly controlled by the aligned fractures due to regional stress and is also influenced by the regional structure units,like fault zones.However,rare studies are applied to systematically analyse the regional effects due to the limited station sampling.This study presented a shear wave splitting analysis based on a dense array(381 stations over two-months records,March 25—May 25,2017)in Binchuan Basin,Yunnan Province,which provides sufficient spatial resolution to resolve the problem.Binchuan Basin is situated northwest of Yunnan Province,close to the city of Dali and the Red River fault.Subject to the strong regional stress caused by the eastern extrusion of the Tibetan Plateau,a set of faults formed in and around the basin,intersecting with each other.Some major faults are nearly perpendicular to the direction of the maximum horizontal principal stress.The misalignment between the strike of the faults and the regional stress provides a unique opportunity to differentiate the contribution of the two mechanisms.Additionally,frequent local earthquakes offer abundant data for shear wave splitting analysis.We manually picked 9819 S-wave arrivals and measured the shear wave splitting parameters using MFAST(Multiple Filter Automatic Splitting Technique),a shear wave splitting method that can automatically assess the quality of the measurements using cluster analysis and a series of quality control criteria.We obtained 831 high-quality shear wave splitting measurements that spread across 173 stations.Our results show that(1)the average polarization of the fast shear waves is NNW(N17.17°±4.64°W),which is consistent with the direction of the maximum horizontal principal stress that is obtained from analysis of GPS data and focal mechanism of earthquakes in a broader region(Yunnan or Sichuan-Yunnan);(2)in spatial,the polarization of the fast shear wave on stations nearby the faults shows patterns related to the faults′strike,indicating a strong regional influence from the f

关 键 词：上地壳各向异性 S波分裂 地方震 密集地震台阵 断裂带 

分 类 号：P315[天文地球—地震学] P541[天文地球—固体地球物理学]