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《Geotectonica Et Metallogenia》 2010-04
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Subsidence Center Migration of the Huanghua Depression in Cenozoic:Evidence of Numerical Modeling

HU Caizhi1,ZENG Zuoxun1,2,REN Jianye3,QI Peng3,LI Zhiyong1,2 and HU Ye1(1.Faculty of Earth Science,China University of Geosciences,Wuhan 430074,Hubei,China;2.Huazhong Research Center of Tectonic Mechanism,Wuhan 430074,Hubei,China;3.Faculty of Earth Resources,China University of Geosciences,Wuhan 430074,Hubei,China)  
Basin formation mainly results from subsidence.The subsidence history of a basin contains huge information such as regional dynamic settings,structural attribution of basin,provenance characteristic,fluid dynamic,and so on.Isopach change is positive correlation to the amount of subsidence range variety and can be used to investigate the paleo-relief,while the paleo-relief reflects the subsidence center of the basin.Based on thorough analyses of documents available and the new seismic data,the authors mapped the isopach maps of each stage of Cenozoic and rebuild the paleo-relief of the Huanghua depression.It is most likely that the subsidence center of the Huanghua depression in Cenozoic migrated northwards along the Cangdong fault and then eastwards.A numerical modeling has been carried out to stimulate the structural subsidence of the Huanghua depression in Cenozoic.It is suggested that activity of the boundary faults bounding the basin was the main mechanism for the migration,whereas the activity of the faults was droved by the stresses of the collision between the Eurasia and India plate,and the subduction of the Izanaqi and Philippine plate underneath the Eurasia plate.First,the Cangdong Fault formed small pull-apart sag at the bendding part.Secondly,the activity of the Lanliao fault led to the northwards migration of the subsidence center along the Cangdong fault.And finally,turned eastwards and reached the largest subsidence center nowadays-the Qikou sag.
【Fund】: 中石油大港油田公司“歧口富油气凹陷结构构造、层序地层与沉积体系研究”项目基金资助
【CateGory Index】: P542.1
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