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《North China Earthquake Sciences》 2011-02
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Study on Upper Mantle Velocity Structure and Tectonic of the Capital Area

WANG Shuai-jun1,2,WANG Fu-yun2,ZHANG Cheng-ke2,HUANG Can3,YANG Ya-qiong4,QI Lang1 (1.University of Science and Technology of China,Hefei 230026,China;2.Research Center of Exploration Geophysics,CEA,Zhengzhou 450002,China;3.Zhengzhou seismic station,Zhengzhou 450062,China;4.Earthquake Administration of Hebei Province,Shijiazhuang 050022 China)  
On the basis of observation data of several seismic sounding profiles and model data of multiple profiles section,this paper presents depth contour of the crystalline basement and that of Moho discontinuity of the Capital area,studies the deep crust velocity structure and the tectonic of this area.The deep crust velocity structure and tectonic show strong lateral heterogeneity,shallow basement faults develops well.The Moho surface contour shows the general characteristics of gradual deepening trend from east to west.The highest gradient zone is near Pinggu and Tangshan area in where deep crustal fault zone may exist with low velocity body along the fault zone.
【Fund】: 国家发展与改革委员会“城市活断层试验探测”项目(2004—1138);; 2004—2010年国家科技基础条件平台建设项目共同资助
【CateGory Index】: P315.2
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