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《Geotectonica Et Metallogenia》 2007-03
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CENOZOIC SUBSIDENCE IN BOHAI BAY BASIN:CHARACTERISTICS AND DYNAMIC MECHANISM

GUO Xingwei1,2, SHI Xiaobin1, QIU Xuelin1, WU Zhiping3, YANG Xiaoqiu1,2 and XIAO Shangbin1(1. CAS Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, GD 510301, China; 2. Graduate School of Chinese Academy of Sciences, Beijing 100039, China; 3. Faculty of Geo-Resource and Information, Petroleum University, Dongying, SD 257061, China)  
The characteristics of development and distribution of Cenozoic faults, amount of extension, and the temporal-spatial variation rules for subsidence of sediments in Bohai Bay Basin were analyzed based on previous study results. Analysis of the deep structures was made to investigate the dynamic mechanism for the Cenozoic subsidence. The results show that in the uplifting period development of faults controls the transition of deposition or subsidence centers, while at the end of the depressing period, accelerated subsidence whose center is Bozhong Depression occurs and shows a tendency of transition from the center to its adjacent depressions. It can be concluded that development of faults, deposition, and subsidence was controlled by the stress field generated from the plate movement, and subsidence of sediments was resulted from the horizontal extension and vertical thermal thinning of lithosphere in the uplifting period. The accelerated subsidence of sediments in the postrift uplifting period may result from the vertical change in density of the lithosphere and its following quick thermal decay.
【Fund】: 国家自然科学基金项目(编号40676041 40204006);; 国家973项目(G2000046701);; 中国科学院南海海洋研究所与广州地球化学研究所边缘海地质重点实验室基金项目(MSGL0511)
【CateGory Index】: P736.5
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4 Weimi CHEN Xin M.A.Menzies 1)(Changsha Institute of Geotectonics, Academia Sinica, Changsha, Hunan, 410013, P.R.China) 2)(Department of Geology, Royal Holloway, University of London. Egham, Surrey TW20 OEX, UK);GEOGRAPHIC VARIATIONS OF MAJOR ELEMENTS FOR PERIDOTITIC XENOLITHS IN RELATION TO CRUST/LITHOSPHERE AGE AND THICKNESS IN EASTERN CHINA[J];Geotectonica Et Metallogenia;1993-03
5 XIAO Shang bin 1, GAO Xi long 2, JIANG Zai xing 1, QIAO Han sheng 3 (1. University of Petroleum, Shandong 257062, China) (2. Shengli Petroleum Administration Bureau, Shandong Dongying 257200, China) (3. Research Institute of Petroleum Explorati;CENOZOIC DEXTRAL STRIKE-SLIP MOTION IN BOHAI BAY BASIN AND ITS MEANING TO PETROLEUM GEOLOGY[J];Geotectonica Et Metallogenia;2000-04
6 SHI Bu-qing 1 ,TIAN Zai-yi 1 ,ZHENG Feng-yun 2 ,ZHOU Yao-qi 3 ,ZHANG Da-gang 3 ,WU Zhi-ping 3 (1.CNPC Key Laboratory for Oil and Gas Re servoirs,Beijing100083,China;2.E &D Research Institute of Zhongyuan Petroleum Co;QUANTITATIVE RELATION BETWEEN MAGM ATISM AND EXTENSION IN CONTINENTAL SEDIME NTARY BASINS:AN EXAMPLE FROM JIYANG DEPRESSION,BOHAI BAY BASIN[J];Geotectonica Et Metallogenia;2001-03
7 WU Kong-you,ZHA Ming and HONG Mei(University of Petroleum,Dongying S handong257061,China);STRUCTURAL MODELS OF UNCONFORMITY AND RECURRENT DIAGENESIS OF SEMI-WEATHERING ROCK IN JUNGGAR BASIN[J];Geotectonica Et Metallogenia;2003-03
8 WANG Shihu~(1,2), XIA Bin~1, CHEN Genwen~1, JIANG Zhaixin~3, XIAO Shangbin~3 and YU Junfeng~1 hemistry & South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, GD 510640, China; 2. Shengli Oil Field Corp., Dongying, SD 257001, China; 3. Resource and Information College, University of Petroleum, Dongying, SD 257061, China);CHARACTERISTICS OF JIYANG DEPRESSION AND MECHANISM OF BASIN FORMATION[J];Geotectonica Et Metallogenia;2004-04
9 CAO Jiebin 1, ZHOU Zuyi 1, WU Nengyou 2, ZHONG Guangfa 1 and WANG Liaoliang 2 (1. Laboratory of Marine Geology, Tongji University, Shanghai 200092, China; 2. Guangzhou Bureau of Marine Geological Survey, Guangzhou, GD 510760, China);LITHOSPHERIC CHARACTERISTICS AND EFFECTIVE ELASTIC THICKNESS OF WESTERN ZENGMU BASIN, SOUTH CHINA SEA: CONSTRAINTS FROM TECTONIC MODELING[J];Geotectonica Et Metallogenia;2005-03
10 Wang Huifen Yang Xuchang Zhu Bingquan Fan Sikun Dai Tongmu(Institute of Geochemistry, Academia Sinica);K-Ar GEOCHRONOLOGY AND EVOLUTION OF CENOZOIC VOLCANIC ROCKS IN EASTERN CHINA[J];Geochimica;1988-01
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