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《Chinese Journal of Geophysics》 2013-03
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Discussion on the special gravity field across the north part of Middle Qinling Mt

WANG Qian-Shen1,TENG Ji-Wen1,ZHANG Yong-Qian1,WEN Wu1,HUA Chang-Cai2 1 Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2 Institute of Geophysics,China Earthquake Administration,Beijing 100081,China  
In this paper,we discussed the special gravity anomaly in the Xianyang-Middle Qinling mountain section in the synthetical geophysical profile from Yulin to Chongqing.Our results suggest that the Northern Qinling fault lies in the gravity anomaly section.The shallow part of the Northern Qinling fault extends in a slightly north-dipping direction with a dip about 70 degrees,and the deep part dips slighty to the south with a dip of 70~80 degrees,while the middle part of it is almost in vertical direction.The big gravity anomaly zone may be caused by the Cenozoic sediments with thickness of 6km and width of 40km in the upper crust.The formation of the Northern Qinling fault belt and the thick sedimentary strata may result from the complicated tectonic movement,especially the thrust of North China plate and the Qinling orogenic movement.
【Fund】: 国家自然科学基金重点项目(90914012)资助
【CateGory Index】: P312
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