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《Chinese Journal of Geophysics》 2005-06
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Three-dimensional crustal gridded structure of the Capital area

JIA Shi-Xu~1,QI Cheng~2,WANG Fu-Yun~1,CHEN Qi-Fu~3,ZHANG Xian-Kang~1,CHEN Yong~31 Research Center of Exploration Geophysics,China Earthquake Administration,Zhengzhou 450002,China2 Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China3 Center for Analysis and Prediction,China Earthquake Administration,Beijing 100036,China  
After unified reprocessing of the 18 DSS profile data that are got in various periods in the Capital area,a digital crust model of velocity grid is obtained with sampling density 0.25°×0.25°×(2~5)km.Through 3-D data visualization,images of slice sections in different strikes and at depths are produced.Based on these images,the tectonic characteristics of the three main geological units,which control the crust in the Capital area including the Yanshan uplift in north,the Taihang uplift in southwest and the rift-depression basin in southeast,and the tectonic features of the contact zone——the Zhangjiakou-Bohai Sea seismic zone are studied from various aspects.Furthmore,the relation between the inner structure of the crust in the Capital area and the generation of catastrophic earthquakes is studied.
【Fund】: 国家自然科学基金重点项目(40234038);; 基础研究重大项目前期研究专项(2001CCA02100);; 地震科学联合基金(105078 101026)资助
【CateGory Index】: P315.7;
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