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《Acta Sedimentologica Sinica》 2012-01
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Analysis on Controlling Factors of Marine Sequence Stratigraphy Evolution in Pearl River Mouth Basin

CHEN Wei-tao1 DU Jia-yuan1 LONG Geng-sheng1 ZHANG Shang-feng2 LI Xiang-yang2(1.Shenzhen Branch of CNOOC Ltd.,Guangzhou 510240;2.College of Geosciences,Yangtze University,Jingzhou,Hubei 434023)  
The Pearl River Mouth basin transformed to a kind of quasi-passive continental margin basin from a continental rifted lake basin after Nanhai movement,and then a set of continental-oceanic transitional facies formations and marine formations which are now the main oil-production formation formed in Pearl River Mouth basin.The analysis on controlling factors of these sets of formations is useful to the third-order sequence stratigraphy division and correlation,and helpful to understand the type and structure of each sequence.Based on the analysis of marine sequence type and developing models of Zhuhai Formation to Yuehai Formation,the controlling factors of marine sequence stratigraphy evolution in Pearl River Mouth Basin are analyzed according to its configuration.It is considered that the tectonic movement,paleogeographic framework,relative sea-level change and sediment supply are the main controlling factors of marine sequence stratigraphy evolution.But these four factors have different effects at different times.The tectonic movement and paleogeographic framework play an important role to the development of sequence stratigraphy from late Oligocene to early Miocene when the basin framework made a great adjustment.Three important movements happened during the period of marine formation forming: the Nanhai movement and the Baiyun movement made the basin framework changed,and controlled the early depositional filling in the basin;The Dongsha movement made parts of basin serious uplift and denudation.These three movements all formed regional unconformities which make up of the second-order sequence boundaries.The influence of paleogeographic framework on the sequence stratigraphy happened in the early period of marine sequence forming,which include the influence of palaeouplift topography,depression topography during the fault-depression stage and shelf breaks.During the peaceful period without tectonic movement,relative sea-level change and sediment supply become the main controlling factors.There is relative wide and smooth continental shelf in Pearl River Mouth Basin,and different types of sequence formed due to the degree of relative sea level fall.When there is a significantly large fall in sea level,reaching to shelf break,a type 1 unconformity develops,such as sequence boundary SB21、SB13.8 and SB10.5 in Pearl River Mouth Basin.When the sea level falling is of lesser magnitude,not reaching to shelf break,a type 2 unconformity develops,such as sequence boundary SB11.7,SB8.5 and SB6.3.In the early period of marine sequence forming,there are three kinds of sediment supply which are Paleo-Pearl River delta,Hanjiang delta and Dongsha uplift;but from late stage of Zhujiang Formation,the sediment supply of Paleo-pearl River delta become the main resources.Whereas the influence area of Paleo-Pearl River delta and other sediment supplies made the same sequence present different characters at different places.
【Fund】: 十一五国家科技重大专项(编号:2008ZX05023-002)资助
【CateGory Index】: P736
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【Citations】
Chinese Journal Full-text Database 10 Hits
1 JI You-Liang1,2 DU Jin-hu3 ZHAO Xian-zheng4ZHANG Yi-ming4 ZHANG Rui-feng4 (1.Petroleum University of China, Beijing 102249; 2.Tongji University, School of Ocean and Earth Science, Shanghai 200092; 3.PetroChina, Beijing 100724; 4.Huabei Oilfied Company, PetroChina, Renqiu, Hebei 062552);Sequence Stratigraphy Models and Controlling Factors of Eogene in Raoyang Depression[J];Acta Sedimentologica Sinica;2007-02
2 WANG Fuguo1,MEI Lianfu2,SHI Hesheng3,YU Shuiming3 and WU Ming1(1.Graduate School,China University of Geosciences,Wuhan 430074,Hubei,China;2.MOE Key Laboratory of Tectonics and Petroleum Resoures,China University of Geosciences,Wuhan 430074,Hubei,China;3.China National Offshore Oil Corporation Ltd.Shenzhen,Guangzhou 510240,Guangdong,China);STRUCTURAL STYLES OF PALEOGENE IN ZHU 1 DEPRESSION OF PEARL RIVER MOUTH BASIN[J];Geotectonica Et Metallogenia;2008-04
3 Pang Xiong 1 , Chen Changmin 1 , Peng Dajun 2 , Zhu Ming 1 , Shu Yu 1 , He Min 1 , Shen Jun 1 , Liu Baojun 1 1.CNOOC Ltd. Shenzhen,Guangzhou 510240,China 2.Chengdu University of Technology, Chengdu 610059, China;Sequence stratigraphy of Pearl River Deep-water Fan System in the South China Sea[J];Earth Science Frontiers;2007-01
4 Xu Shice;Yang Shaokun;Huang Lifen (Scientific Research Center,China Offshore Oil Nanhai East Corporation,Guangzhou,510240);THE APPLICATION OF SIQUENCE STRATIGRAPHY TOSTRATIGRAPGHIC CORRELATION[J];EARTH SCIENCE FRONTIERS;1995-03
5 PANG Xiong1), PENG Dajun2), CHEN Changmin1), ZHU Ming1), HE Min1), SHEN Jun1), LIU Baojun1)1) CNOOC Ltd. Shenzhen, Guangzhou, Guangdong, 5102402) Chengdu University of Technology, Chengdu, Sichuan, 610059;Three Hierarchies “Source-Conduit-Sink” Coupling Analysis of the Pearl River Deep-water Fan System[J];Acta Geologica Sinica;2007-06
6 LIU Zengqin 1,2,WANG Yingmin1,2,SHI Hesheng3,DU Jiayuan3(1 School of Resource and Information Technology,China University of Petroleum,Beijing 102249,China;2 State Key Laboratory of Petroleum Resource and Prospecting,China University of Petroleum,Beijing 102249,China;3 Shenzhen Branch,CNOOC,Guangzhou 510240,China);SEQUENCE STRATIGRAPHY DIVISION AND SEDIMENTARY FACIES DISTRIBUTION OF LOWER ZHUJIANG FORMATION IN HUIZHOU AREA[J];Marine Geology Letters;2010-05
7 Zhong Jianqiang(South China Sea Institute of Oceanology. Academia Sinica,Guangzhou 510301);CHARACTERISTICS OF GEOLOGIC STRUCTURE AND BASIN EVOLUTION IN PEARL RIVER MOUTH BASIN[J];Transaction of Oceanology and Limnology;1994-01
8 DONG Wei1,LIN Chang-song1,QIN Cheng-gang2,XIE Li-hua1,YANG Xiao-fa1,CUI Li-ye1,ZHANG Bo1(1.School of Energy Resources,China University of Geosciences,Beijing 100083,China;2.Shenzhen Institute of CNOOC Limited,Guangzhou,Guangdong 510240,China);High Resolution Sequence Framework,Depositional Pattern and Litho-Stratigraphic Traps of Hanjiang Formation in Panyu Uplift,Pearl River Mouth Basin[J];Geoscience;2008-05
9 Wang Chunxiu (China Offshore Oil Exploration and development Research Center, Hebei);SEQUENCE STRATIGRAPHIC ANALYSIS OF MARINE MIOCENE FORMATIONS IN THE PEARL RIVER MOUTH BASIN AND ITS SIGNIFICANCE[J];;1996-05
10 Qin Guoquan (Nanhai East Institute of CNOOC Research Center, Guangzhou);LATE CENOZOIC SEQUENCE STRATIGRAPHY AND SEA-LEVEL CHANGES IN PEARL RIVER MOUTH BASIN,SOUTH CHINA SEA[J];;2002-01
【Co-citations】
Chinese Journal Full-text Database 10 Hits
1 CHEN Jun,XU Guo-qiangCollege of Energy Resources,Chengdu University of Technology,Chengdu 610059,China;Type and distribution characterestics of the faults in the B depression of the Zhujiangkou basin,China[J];Journal of Chengdu University of Technology(Science & Technology Edition);2008-03
2 YU Hai-bo (Key Laboratory of Exploration Technologies for Oil and Gas Resources(Yangtze University),Ministry of Education,Jingzhou 434023) DU Jia-yuan (Key Laboratory of Exploration Technologies for Oil and Gas Resources (Yangtze University),Ministry of Education,Jingzhou 434023;Shenzhen Branch of CNOOC Ltd.,Guangzhou 510240);Tide-influenced Delta Deposits of Wellblock A in Lower Zhujiang Formation of Pearl River Mouth Basin[J];Journal of Yangtze University(Natural Science Edition);2011-01
3 SANG Shu xun 1 LI Zhuang fu 1 FAN Bing heng 1 CHEN Shi yue 2 1 (College of Mineral Resources and Environment Sciences, China College of Mining and Technology, Xuzhou Jiangsu 221008) 2 (Department of Resources, University of Petroleum,;Sequence Stratigraphic Framework and Correlation of Coal and Rock Seams --Sequence stratigraphy applied to coal exploration inYangqu,Shanxi[J];Acta Sedimentologica Sinica;2001-04
4 TANG Song SHAO Lei ZHAO Quan-hong (Key Laboratory of Marine Geology, Ministy of Education,Tongji University, Shanghai 200092);Characteristics of Clay Mineral in South China Sea since Oligocene and Its Significance[J];Acta Sedimentologica Sinica;2004-02
5 CHEN Guo-jun1,2 LV Cheng-fu1,2 LI Yu-lan1,2 HE Shi-bin 3WANG Tian-qi4 LIU De-wen1,2 DU Gui-chao1,2(1.Key Laboratory of Gas Geochemistry,Chinese Academy of Sciences,Lanzhou 730000;2.Graduate School of Chinese Academy of Sciences,Beijing 100049;3.CNOOC Research Center,Beijing 100027;4.Research Institute of Petroleum Exploration and Development,CNPC,Lanzhou 730030);Analysis of the Oil-and Gas-Bearing Turbidite Within Wenchang Formation in Enping Depression,Pearl River Mouth Basin,China[J];Acta Sedimentologica Sinica;2008-05
6 WU Shi-guo QIN Yun-shan(Institute of Oceanology,Chinese Academy of Sciences,Key Laboratory of Marine Geology and Environment,Qingdao Shandong 266071);The Research of Deepwater Depositional System in the Northern South China Sea[J];Acta Sedimentologica Sinica;2009-05
7 XIE Li-hua1,2 ZHANG Bo3 QIN Cheng-gang3 WANG Yan-fei3 CHEN Sheng-hong3 GAO Peng3(1.School of Earth and Space Sciences,Peking University,Beijing 100871;2.School of Energy Resources,China University of Geosciences,Beijing 100083;3.Technology Department,Shenzhen Branch Company,CNOOC Ltd.,Guangzhou 510240);Forced Regression and Normal Regression Deposition of Basin with Continental Shelf Slope-break:A case study on Zhujiang and Hanjiang Formations of Pearl River Mouth Basin[J];Acta Sedimentologica Sinica;2009-06
8 LAI Wei-cheng 1) , JIANG Pei-hai 2) , XU ·· Chang-gui 1) , and LIU Fu-ping 1) ( 1)Technical Department of CNOOC China, Limited-Tianjin, Tianjin, 300452; 2)Explaratory Department CNOOC, China,Beijing,100027 );DISCUSSION ON THE UNIFICATION AND INHERITANCE BETWEEN TRADITIONAL STRATIGRAPHY AND SEQUENCE STRATIGRAPHY[J];Journal of Stratigraphy;2004-04
9 HE Wei-jun,XIE Jin-you,LIU Xin-yu and LI Shan-shanZhanjiang Branch of CNOOC Ltd.,Zhanjiang 524057;FORAMINIFERAL BIOSTRATIGRAPHY AND SEDIMENTARY ENVIRONMENT RECONSTRUCTION BASED ON PALEONTOLOGICAL DATA FROM BORE HOLE DF1-1-11,YINGGEHAI BASIN[J];Journal of Stratigraphy;2011-01
10 LI Qian-yu1,2,ZHAO Quan-hong1,ZHONG Guang-fa1,JIAN Zhi-min1,TIAN Jun1,CHENG Xin-rong1,CHEN Mu-hong3 1.State Key Laboratory of Marine Geology,Tongji University,Shanghai 200092,China2.School of Earth and Environmental Sciences,The University of Adelaide,Adelaide SA5005,Australia3.South China Sea Institute of Oceanology,Chinese Academy of Sciences,Guangzhou 510301,China;Deep Water Ventilation and Stratification in the Neogene South China Sea[J];Earth Science(Journal of China University of Geosciences);2008-01
【Secondary Citations】
Chinese Journal Full-text Database 10 Hits
1 XIA Zai-lian,XU Guo-qiang,LIU Shu-gen, LIU Shun,LI Zhi-wuState Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology,Chengdu 610059,China;A structural style analysis of the eastern Micangshan and Dabashan foreland zone,China[J];Journal of Chengdu University of Technology(Science & Technology Edition);2008-01
2 Li Wenxiang.;Mineral identification Capability of Log interpretation Model[J];WELL LOGGING TECHNOLOGY;1994-04
3 WANG Guo zhi WANG Cheng shan ZENG Yun fu ZHAO Xi kui (Chengdu University of Technology,Chengdu 610059 P.R.China);The Uplift of the Western Yunnan Plateau and the Sedimentary Response of the Yinggehai Basin[J];ACTA SEDIMENTOLOGICA SINICA;2000-02
4 PENGDa-jun 1PANGXiong 2CHENChang-min 2YUShu 2 YEBing 1 GANJi-gang 1 WUChang-rong 1 HUANG Xian-lu 1 1(Chengdu University of Technology, Chengdu610059) 2(Tachnology Department, Shenzhen, CNOOC Ltd, Guangzhou 510240);From Shallow-water Shelf to Deep-water Slope——thestudy on deep-water fan systems in South China Sea[J];Acta Sedimentologica Sinica;2005-01
5 LIN Ge, WANG Yue-jun, LI Zi-an(Changsha Institute of Geotectonics, Academia Sinica, Changsha 410013, China);THE STRUCTURAL PATTERNS AND GAS RESERVIORS-FORMING IN SEDIMENTARY BASINS[J];GEOTECTONICA ET METALLOGENIA;1999-03
6 LI Zhiwu1, LIU Shugen1, LUO Yuhong2, LIU Shun1 and XU Guoqiang1 (1. Chengdu University of Technology, Chengdu, SC 610059, China; 2. Central Sichuan Mining District, Southwest Oil and Gas Field Branch Company, PetroChina, Suining, SC 629000, China);STRUCTURAL STYLE AND DEFORMATIONAL MECHANISM OF SOUTHERN DABASHAN FORELAND FOLD-THRUST BELT IN CENTRAL CHINA[J];Geotectonica Et Metallogenia;2006-03
7 Lin Changsong 1 Pan Yuanlin 2 Xiao Jianxin 1 Kong Fanxian 2 Liu Jingyan 1 Zheng Herong 2 (1. Department of Energy Resources, China University of Geosciences, Beijing100083, China; 2. Shengli Oil Administration Bureau, Dongying257001, China);STRUCTURAL SLOPE-BREAK ZONE: KEY CONCEPT FOR STRATIGRAPHIC SEQUENCE ANALYSIS AND PETROLEUM FORECASTING IN FAULT SUBSIDENCE BASINS[J];;2000-03
8 LI Si tian 1, PAN Yuan lin 2, LU Yong chao 1, REN Jian ye 1, XIE Xi nong 1, WANG Hua 1 (1.Institute of Sedimentary Basin and Minerals, China University of Geosciences, Wuhan430074, China; 2.Shengli Oil Field Limited Company, China Petroleum & Chemical Corporation, Dongying257000, China);Key Technology of Prospecting and Exploration of Subtle Traps in Lacustrine Fault Basins: Sequence Stratigraphic Researches on the Basis of High Resolution Seismic Survey[J];;2002-05
9 LI Qian-yu, ZHENG Hong-bo, ZHONG Guang-fa, WANG Pin-xianLaboratory of Marine Geology, Tongji University, Shanghai200092, China;Tectonic Events Indicated by Late Oligocene Slumped Deposits from the South China Sea[J];;2005-01
10 WANG Lei1,LV Shuang-bing2,ZHU Ying-kang2(1.College of Geosciences,Daqing Petroleum Institute,Daqing,Heilongjiang 163318,China;2.Daqing Oil Field Exploration and Development Institute,Daqing,Heilongjiang 163012,China);Structural pattern of thrust-fold zone in southern Jungger foreland basin and effect on the formation of traps[J];Journal of Daqing Petroleum Institute;2007-06
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