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《Geotectonica et Metallogenia》 2014-01
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Comparison of the Bohai Bay Basin and Subei-South Yellow Sea Basin in the Structural Characteristics and Forming Mechanism

LIU Yin;CHEN Qinghua;HU Kai;WANG Xi;GAO Feng;School of Earth Sciences and Engineering,Nanjing University;School of Earth Sciences and Technology,China University of Petroleum (East China);MLR Key Laboratory of Tectonic Controlled Mineralization and Oil Reservoir,Chengdu University of Technology;Geological Scientific Research Institute of Jiangsu Oilfield Company,SINOPEC;  
The Bohai Bay Basin and the Subei-South Yellow Sea Basin are important petroliferous basins in China and often compared with each other. Although there are many similarities between these two basins,the differences in aspects such as the abundance of the resources,the scale of the oil and gas field and the hydrocarbon evolution degree are significant. The primary cause of these differences is the different regional tectonic background. Based on the geological and geophysical data,we make a comparison of the two basins in several aspects,such as the basin architecture,internal structure,fault activity characteristics,and explore the influence factors and mechanism of the basin formation. We suggest that four main factors controlled the formation of the two basins:(1) The collision between the Yangtze and North China Plate,which happened during the Indosinian,provided the evolution foundation of the Subei-North Yellow Sea Basin. The Bohai Bay Basin evolution history may start earlier than the Subei-North Yellow Sea Basin,at Late Paleozoic.(2) The subduction of the plates in the Marginal Pacific Tectonic Domain beneath the Eurasian Plate had a significant impact on the formation of the two basins.(3) Deep earth thermal activity played an important role in forming of the Bohai Bay Basin,while that was not the reason for the Subei-South Yellow Sea Basin rift.(4) The collision between the Indian Plate and Eurasian Plate caused continuous mass injection over the past ~50 Ma,led to the diffuse asthenospheric upwelling and rifting of the two basins. Combined with the influence factors and the tectonic background,we set up the evolution models of the two basins.
【Fund】: 国家自然科学基金项目(批准号:41373044);; 构造成矿成藏国土资源部重点实验室开放基金(编号:gzck2012005)联合资助
【CateGory Index】: P618.13
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