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《Earth Science(Journal of China University of Geosciences)》 2009-04
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Structure of Crust and Upper Mantle in Tianshui-Wudu Strong Earthquake Region of North-South Tectonic Belt

LAI Xiao-ling1,LI Song-lin1,SONG Zhan-long1,FAN Ji-chang1,LIU Ming-jun1,HE Jia-yong2 1.Geophysical Exploration Center,China Earthquake Administration,Zhengzhou 450002,China 2.Institute of Geophysics,China Earthquake Administration,Beijing 100081,China  
The structure of crust and upper mantle in Tianshui-Wudu strong earthquake region is studied by using DSS data from two cross high resolution refraction /wide angle reflection profiles and corresponding fan profiles.The 2-D result shows that the crust can be vertically divided into two layers:upper crust and lower crust.There exists a low velocity layer in the upper crust with velocity difference of 0.3-0.5 km/s.The depth of Moho is about 46-48 km.There is a strong lateral variation in the lower crust along the NE Tianshui-Wudu profile.And along the NW Chengxian-Wushan profile,there are some evidences showing that the Moho and C discontinuities are changed by substances from the deep layer.The 3-D result shows that there is a fault with near NS strike at the depth of 7-11 km near 105°E.The velocities at the two sides of this fault are quite different:low velocity at the west side and high velocity at the east side.This NS fault is very close to the deep fault of 2-D profile.All the large earthquakes occurred near 105°E and formed a NS belt.
【Fund】: 国家自然科学基金项目(Nos.40774043 40674043 90814001);; 财政部“南北地震带紧急强化震情跟踪”专项经费;; 中国地震局地球物理勘探中心论著RCEG0806资助
【CateGory Index】: P631.4
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