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《Chinese Journal of Geophysics》 2010-05
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The Jinzhong transition belt and its geological significance by receiver function in Shanxi region

LI Chuan-Jin~(1,2),XU Pei-Fen~1,SUN Yong-Jun~(1,2),JIA Jian-Xi~3 1 Key Laboratory of the Study of Earth's Deep Interior,Institute of Geology and Geophysics,Chinese Academy of Sciences, Beijing 100029,China 2 Graduate University,Chinese Academy of Sciences,Beijing 100049,China 3 Seismological Bureau of Shanxi Province,Taiyuan 030021,China  
Seismic data collected by Shanxi Digital Seismic Network during a six-year time period were used to compute crustal thickness using the receiver function method and H-k search.The results show that at the northern margin of Pingyao Basin in Shanxi region,there exists a transition belt along the line between Wenshui and Jinzhong,called Jinzhong transition belt.The belt acts as a dividing line between the south thin crust (about 37~40 km) and the north thick crust (about 41~45 km) trending in NEE direction.We consider this transition belt being related to early precambrian basement structure and an important tectonic boundary inside the North China Craton.In this region,the basement structure is well-preserved and the crust is relatively thick.
【Fund】: 中国科学院知识创新工程重要方向项目(KZCX2-YW-103);; 国家自然科学基金面上项目(40874025)共同资助
【CateGory Index】: P315
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