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《Chinese Journal of Geophysics》 2006-01
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Features of deep crustal structure beneath the Wutai mountain area of Shanxi province

ZHAO Jin-Ren, ZHANG Xian-Kang, ZHANG Cheng-Ke, ZHANG Jian-Shi, LIU Bao-Feng, PAN Su-ZhenGeophysical Exploration Center, China Earthquake Administration, Zhengzhou 450002, China  
The crustal structure was investigated with Deep Seismic Sounding(DSS) data obtained from wide angle reflection/refraction profiles which extent through the Shanxi faulted-depression belt and the Wutai mountain area. The results show that the crust represents obviously layered structures in the areas. The boundary interface between lower and upper crust is determined by means of reliable reflected wave group P_3, which can be traced continuously in the crust. The thickness of the upper crust is 23~28km and the depth of Moho is 39~43km. The deepest Moho of this region located beneath the Wutai mountain area. In the Wutai mountain and its adjacent areas, the crust structures have strong inhomogeneous characteristics. The existence of abnormal low-velocity bodies in the uppercrust in a larger scope and strong reflected wave groups in the crust maybe regarded as a sign of magma activity in the deep crust. Based on breaking of interior crust interfaces and local discontinuation of the seismic wave group Pm along with existence of deep faults, it is suggested that the crust in this region has experienced violent pressure, deformation and tectonic activities, which resulted in complex topography and anomalous structural features within the crust.
【Fund】: 国家自然科学重点基金项目(40334040)资助;; 中国地震局地球物理勘探中心论著编号RCEG200403·
【CateGory Index】: P542.5
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