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《Acta Sedimentologica Sinica》 2010-01
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Architecture and Origin of Deepwater Sinuous Channel on the Slope of Northern South China Sea

YUAN Sheng-qiang1,2,3 CAO Feng4 WU Shi-guo2 YAO Gen-shun5 WANG Hai-rong6 LI Li5 ( 1. State Key Laboratory of Enhanced Oil Recovery,Research Institute of Petroleum Exploration and Development,Beijing 100083; 2. Key Laboratory of Marine Geology and Environment,Institute of Oceanology,Chinese Academy of Sciences,Qingdao Shandong 266071; 3. Graduate School of Chinese Academy of Sciences,Beijing 100049; 4. Research Institute of Petroleum Exploration & Development ,Beijing 100083; 5. Hangzhou Institute of Geology,PetroChina Hangzhou 310023; 6. China University of Geosciences,Beijing 100083)  
The deepwater channel is one important element of deepwater sedimentary system,and is becoming more important to the oil industry for its potential hydrocarbon reserve. Most of the deepwater channels were buried in the submarine sedimentary formation,and are difficult to observe and study directly. Based on the new required 2D and 3D seismic data,this paper used attribute analysis technologies,likewise 3D ESP coherence time slices( flattened on the seafloor) ,RMS and 3D visualization to realize and study the deepwater channel developed on the slope of northern South China Sea. This channel was a deepwater sinuous channel developed in Pleistocene period,and was formed by the turbidite flow from the Indo-China peninsula. The channel is SW-NE extend,the lateral erosional features is apparent. The 3D amplitude visualization map shows that the axis fill of the channel is high amplitude reflection,and was supposed to be sand-rich fill,the other part of the channel fill is low amplitude reflection,and was supposed to be mud-rich fill,which are similar with the deepwater channel drilled in the world. The deepwater sinuous channel has complex inner fill and composition architecture,the sand and shale layer are always interbedded,the shale layer could either hinder the migration of the flow and form overpressure or be a better seal to the flow,and we should pay more attention to this problem under the exploration and development to deepwater sinuous channel.
【Fund】: 中国科学院重要方向性项目(编号:KZCX2-YW-229);; 国家863高技术项目(编号:2006AA09Z349)项目联合资助
【CateGory Index】: P618.13
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【Citations】
Chinese Journal Full-text Database 6 Hits
1 GAO Zhen zhong 1 HE You bin 1 ZHANG Xing yang 1 ZHAI Yong hong 1 HU Yun yang 2 YANG Hai jun 2 LI Xin sheng 2 LI Yong 2 1 (Department of Geology, Jianghan Petroleum Institute, Jingzhou, Hubei 434102) 2 (Tarim Petroleum Explor;Internal-Wave and Internal-Tide Deposits of the Middle-Upper Ordovician in the Center Tarim Basin[J];ACTA SEDIMENTOLOGICA SINICA;2000-03
2 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
3 PENG Da-jun~(1)PANG Xiong~(2)CHEN Chang-min~(2)ZHU Ming~(2)HUANG Xian-lu~(1)SHU Yu~(2)(1.Chengdu University of Technology,Chengdu610059;2.China National Oceanic Oil company,Shenzhen Branch,CNOOC Guangzhou510240);The Characteristics and Controlling Factors for the Formation of Deep-water Fan System in South China Sea[J];Acta Sedimentologica Sinica;2006-01
4 YUAN Yu-Song~1, YANG Shu-Chun~2, HU Sheng-Biao~3, HE Li-Juan~31 Exploration and Production Research Institute, SINOPEC, Beijing 100083, China2 Beijing Research Center of CNOOC China Ltd., Beijing 100027, China3 Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;Tectonic subsidence of Qiongdongnan Basin and its main control factors[J];Chinese Journal of Geophysics;2008-02
5 YAO Gen-shun1,2,3,YUAN Sheng-qiang1,2,WU Shi-guo1,4,ZHONG Chuang5(1.Key Laboratory of Marine Geology and Environment,Institute of Oceanology,Chinese Academy of Sciences,Qingdao 266071,China;2.Graduate School of Chinese Academy of Sciences,Beijing 100049,China;3.PetroChina Hangzhou Institute of Geology,Hangzhou 310023,China;4.China University of Petroleum(Huadong),Qingdao 266555,China; 5.Luliang Oil Production Company,PetroChina Xinjiang Oilfield Company,Karamay 834000,China );Double provenance depositional model and exploration prospect in deepwater area of Qiongdongnan Basin[J];Petroleum Exploration and Development;2008-06
6 Tao Weixiang~(1,2),He Shibin~2,Zhao Zhigang~2,Ding Fang~2(1.Faculty of Earth Resources,China University of Geosciences,Wuhan,Hubei 430074,China;2.CNOOC Research Center,CNOOC,Beijing 100027,China);RESERVOIR DISTRIBUTION IN DEEPWATER AREA OF THE QIONGDONGNAN BASIN[J];Petroleum Geology & Experiment;2006-06
【Co-citations】
Chinese Journal Full-text Database 10 Hits
1 WU Chang-rong~1,PENG Da-jun~1,PANG Xiong~2,YE Bin~1,SHU Yu~21.College of Energy Resources,Chengdu University of Technology,Chengdu 610059,China;2.Shenzhen Branch of China National Offshore Oil Company Ltd.,Guangzhou 510240, China;An analysis of the structural background of the sedimentation of the Zhujiang deep-water fan system in the South China Sea[J];Journal of Chengdu University of Technology(Science & Technology Edition);2006-03
2 JIN Hui-juan LI Yu-ci FANG Guo-qing (Lanzhou Institute of Geology, Chinese Academy of Sciences, Lanzhou 730000);Internal-wave and Internal-tide Deposits in the Paleostratigraphic Record of the Western Qinling Mountains and Their Origin[J];Acta Sedimentologica Sinica;2002-01
3 WANG Qing-chun~1BAO Zhi-dong~1HE Ping~ 1(University of Petroleum, Beijing 102249) 2(Research Institute of Petroleum Exploration, Huabei Oilfield, Renqiu Hebei 062552);The Generational Mechanism of Orientating Sedimentary Structure by Internal-waves[J];Acta Sedimentologica Sinica;2005-02
4 LIU Bao-jun~(1) YUAN Li-zhong~(1) SHEN Jun~(1) LIAN Shi-yong~(1) HE Min~(1) PANG Xiong~(1) SHU Yu~(1) PENG Da-jun~(2)(1.Shenzhen Corpration,CNOOC,Guangzhou 510240;2.Chengdu University of Technology,Chengdu 610059);Northern Continental Slope Palaeogeomorphology and Deep-water Fan System Response of Pearl River Since 13.8Ma,South China Sea[J];Acta Sedimentologica Sinica;2006-04
5 WANG Ying-min1 WANG Hai-rong1,2 QIU Yan3 PENG Xue-chao3 ZHANG Wen-ming1 LI Wen-cheng3(1.Key Laboratory of Education Ministry for Hydrocarbon Accumulation Mechanism,University of Petroleum,Beijing 102249;2.Basin and Reservoir Research Center,University of Petroleum,Beijing 102249;3.Institute of Guangzhou Marine Geological Survey,Guangzhou 510760);Process of Dynamics and Its Response of Deep-Water Sedimentation[J];Acta Sedimentologica Sinica;2007-04
6 WANG Hai-rong1,2 WANG Ying-min1 QIU Yan3 PENG Xue-chao3 HUANG Qi-zhi4(1.School of Energy,China University of Geosciences,Beijing 100083;2.Basin and Reservoir Research Center,University of Petroleum,Beijing 102249;3.Institute of Guangzhou Marine Geological Survey,Guangzhou 510760;4.China National Oil and Gas Exploration and Development Corporation,Beijing 100083);Development and Its Tectonic Activity's Origin of Turbidity Current Sediment Wave in Manila Trench,the South China Sea[J];Acta Sedimentologica Sinica;2008-01
7 WEI Xiu-guo1,2,3 SHEN Cheng-de1 SUN Yan-min1 YI Wei-xi1(1 Guangdong Institute of Eco-environment and Soil Sciences,Guangzhou 510650;2 Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640;3.Department of Tourism and Environment,Guangdong Institute of Business Studies,Guangzhou 510320);The Study of Stable Carbon Isotope Composition of Riverine Suspended Matter and Soil Erosion of the Pearl River Drainage Basin[J];Acta Sedimentologica Sinica;2008-01
8 LI Xiang-hui1 WANG Cheng-shan2 JIN Wei3 RAN Bo2(1. Department of Earth Sciences, Nanjing University, Nanjing 210093;2.China University of Geosciences, Beijing 100083; 3. Exploration and Development Research Institute, Daqing Oilfield Company Limited, Daqing, Heilongjiang 163712);A Review on Deep-Sea Sedimentation Theory:Significances to Oil-gas Exploration[J];Acta Sedimentologica Sinica;2009-01
9 He You-bin, Gao Zhen-zhong, Guo Cheng-xian, Xu Hui,Dong Gui-yu(School of Earth Sciences, Yangtze University, Jingzhou 434023, Hubei, China);Study on internal-wave and internal-tide deposits of the third member of the Lower Cambrian Balang Formation at Yangjiaping, Shimen[J];Chinese Geology;2005-01
10 WANG Jia-hao1, PANG Xiong2, WANG Cun-wu1, HE Min2, LIAN Shi-yong2 1.Faculty of Earth Resources, China University of Geosciences, Wuhan430074, China 2.CNOOC Ltd. Shenzhen, Guangzhou510240, China;Discovery and Recognition of the Central Diapiric Zone in Baiyun Depression, Pearl River Mouth Basin[J];;2006-02
【Secondary Citations】
Chinese Journal Full-text Database 10 Hits
1 Gao Zhenzhong (Department of Geology, Jianghan Petroleum Institute) K.A.Eriksson (Department of Geological Sciences, VirginiaPolytechnic Institute and State University, USA);Internal-tide Deposits in an Ordovician Submarine Channel, Fincastle, Appalachians, USA[J];Acta Sedimentologica Sinica;1993-01
2 ZHANG Xing yang 1 GAO Zhen zhong 1 YAO Xue gen 2 1(Geoglogy Department of Jiang han Petrdeum Institute,Jingzhou Hubei 434102) 2(Manager Department of Nature Gas Exploration Project of Sichuan and Hubei,Wanxian Sichuan 634000);Internal wave Deposits in the North eastern Rockall Trough,North Atlantic Ocean ——Reinterpretation of deep water sediment waves formation[J];ACTA SEDIMENTOLOGICA SINICA;1999-03
3 Xie Xinong 1\ Li Sitian 1\ Ge Ligang 1\ Zhang Qiming 2 and \ Wang Zhenfeng 2 1\ (China University of Geosciences,Wuhan\ 430074) 2\ (West Oil Company of South China Sea,Zhangjiang\ 524000);Internal Achitectures and Evoluting Model of Bay Fan Delta System in Yanan Sag of Qiongdongnan Basin[J];ACTA SEDIMENTOLOGICA SINICA;1996-03
4 CHEN Guoda(Changsha Institute of Geotectonics, Academia Sinica; International Research Center forGeodepressional (Diwa ) Tectonics and Metallogeny; WG4, Tectono - Magmatic Activization(Diwa ), IAGOD/CTOD, Changsha 410013, China );THE MARGINAL EXTENSIONAL BELT OF EAST ASIA CONTINENT INVESTIGATING THE ORIGINOF A DISCRETE CONTINENTAL MARGIN[J];GEOTECTONICA ET METALLOGENIA;1997-04
5 ZHANG Jian and SHI Yao-lin(The United Laboratory of Calculativ e Geodynamics,Graduate School of th e Chinese Academy of Sciences,Beiji ng100039,China);THERMODYNAMICS MECHANISM OF THE MARGINAL EXTENSIONAL BELT OF EAST ASIA[J];Geotectonica Et Metallogenia;2003-03
6 Wei Kuisheng1 Cui Hanyun2 Ye Shufen1 Li Daliang1 Liu Tieshu2 Liang Jianshe2 Yang Guozhong2 Wu Li1 Zhou Xiaoying1 Hao Yunqing1(1.Department of Energy Resources, China University of Geosciences, Beijing100083, China; 2.Exploration & Production Rese;HIGH-PRECISION SEQUENCE STRATIGRAPHY IN QIONGDONGNAN BASIN[J];;2001-01
7 Gong Zaisheng 1, Yang Jiaming 2, Hao Fang 3, Hu Jianwu 3 (1.China National Offshore Oil Corporation, Beijing100029, China; 2.Institute of Petroleum Exploration and Development, CNOOC, Gaobeidian074010, China; 3.Faculty of Earth Resources, Chi;DIFFERENCE IN NATURAL GAS ACCUMULATION CONDITIONS BETWEEN YINGGEHAI AND QIONGDONGNAN BASINS AND ITS IMPLICATIONS FOR NATURAL GAS EXPLORATION[J];;2001-03
8 SUN Zhen1,ZHONG Zhi-hong2,ZHOU Di11.CAS Key Laboratory of Marginal Sea Geology,South China Sea Institute of Oceanology,Guangzhou510301,China2.Department of Science and Technology,Shenzhen Branch of CNOOC,Guangzhou510240,China;The Analysis and Analogue Modeling of the Tectonic Evolution and Strong Subsidence in the Yinggehai Basin[J];Earth Science(Journal of China University of Geosciences);2007-03
9 ZHENG Yong 1,2, FU Rong-Shan1, XIONG Xiong31 School of Earth Space Science, University of Science and Technology of China, Hefei 230026, China2 Institute of Geophysics, China Earthquake Administration, Beijing 100081, China3 Wuhan Institute of Geodesy and Geophysics, Wuhan 430077, China;Dynamic simulation of lithospheric evolution from the modern China mainland and its surrounding areas[J];Chinese Journal of Geophysics;2006-02
10 XU Zhen1, XU Ming-Jie1, WANG Liang-Shu1, LIU Jian-Hua2, ZHONG Kai1, TONG Wei-Wei11 Department of Earth Sciences, Nanjing University, Nanjing 210093, China2 Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;A study on crustal anisotropy using P to S converted phase of the receiver function:Application to Ailaoshan-Red River fault zone[J];Chinese Journal of Geophysics;2006-02
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