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《Acta Scientiarum Naturalium Universitatis Pekinensis》 2008-03
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Tectonic Subsidence of the Major Cenozoic Basins along the Yingkou-Weifang Fault Zone and Its Response to the Neighbouring Plate Movement

DENG Rongjing1,2,3,XU Bei3,QI Jiafu4,HAO Lihua2,ZHANG You5 1Postdoctoral Center of China University of Geosciences,Beijing 100083;2CNOOC Beijing Research Center,Beijing 100027;3School of Earth and Space Sciences,Peking University,Beijing 100871;4China Petroleum University,Beijing 102249;5CNOOC Bohai Petroleum Research Institute,Tianjin 300452  
Yingkou-Weifang fault zone is a part of central segments of Tanlu fault zone,along which several Cenozoic basins,such as Weibei,Laizhouwan,Huanghekou,Bozhong,Bodong,Liaodong,Liaozhong are developed.Tectonic subsidence calculation and mapping demonstrate that there are four types of tectonic subsidence curve,each corresponding to different basin style.Tectonic subsidence rate along the fault zone indicates its movement migrated from the two ends to the central.The convergence rates and their directions of Pacific plate and India plate towarding Eurasian plate dominate the tectonic evolution and its average tectonic subsidence change.Bohaiwan Cenozoic basin is a superimposed basin of pull-apart basin and an active extension basin.
【Fund】: 教育部博士点基金资助项目(20020001055)
【CateGory Index】: P548
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