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《Journal of Palaeogeography》 2005-01
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Sedimentary facies of the Yanchang Formation of Upper Triassic and petroleum geological implication in southwestern Ordos Basin

Fu Jinhua 1,2 Guo Zhengquan 2 Deng Xiuqin 2 1 Department of Geology,Northwest University,Xi'an 710069,Shaanxi2 Research Institute of Petroleum Exploration and Development,Changqing Oilfield Company,PetroChina,Xi'an 710021,Shaanxi  
In the Yanchang Formation of Triassic in the Ordos Basin mainly two sedimentary systems are developed:the northeastern and southwestern systems.It has been proved that the northeastern sedimentary system is a river delta system through abundant research data.However,the southwestern system is little studied as there has been only limited efforts in exploration.Based on the latest drilling and outcrop data,it has been concluded that the southwestern sedimentary system in the Ordos Basin is an alluvial fan-fan delta system and the alluvial fan,fan delta and lake facies or turbidite facies were developed.The alluvial fan is typical in the sections of Pingliang Kongdongshan and Ruishuihe River.The fan delta and lake facies or turbidite facies are proved by observation on the drilling sections in the study area.The main reservoirs include the intervals Chang 6 to Chang 8 and the strata are preserved integration with relatively high intensity of drilling efforts.The subaqueous distributary channel is the main type of the fan delta front while the channel mouth bar is developed locally.The turbidite sandstone is mainly thick-bedded.Fan delta front subfacies was best developed during the Chang 8 Subage.Three delta front sandbody belts are formed from southwest to northeast and they are the important areas where hydrocarbon accumulates.The turbidite system was well developed in the Chang 7 Subage because the lake basin subsided,the periphery was uplifted strongly and the lakeshore was very steep.The fan delta was developed again because the lake regression occurred during the Chang 6 Subage,but the scale was smaller than that of the Chang 8 Subage.The fan delta front sandbody is the most advantageous zone of petroleum accumulation because of its great thickness,coarse grainsize,well sorting and good physical properties.
【CateGory Index】: P512.2;P618.13
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2 JI Liming~(1,2),XU Jinli~(3)) and SONG Zhiguang~(2)) 1 ) Key Laboratory of Petroleum Resources Research,Institute of Geology and Geophysics,Chinese Academy of Sciences,Lanzhou 730000 2) State Key Laboratory of Organic Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640 3) Geological Sciences Institute,Sinopec Shengli Oilfield Company,Dongying 257015;LACUSTRINE CYANOBACTERIA FROM THE YANCHANG FORMATION IN ORDOS BASIN AND ITS IMPLICATION OF OIL SOURCE[A];[C];2013
3 ZHANG Xiao-li~(1,2),DUAN Yi~1,HE Jin-xian~(1,2),WU Bao-xiang~1,XU Li~(1,2) (1.Key Laboratory of Petroleum Research of Institute of Geology and Geophysics, Chinese Academy of Sciences,Lanzhou 730000;2.Graduate School, Chinese Academy of Sciences,Beijing 100049,China);Characteristics of the Sedimentary Microfacies and the Oil and Gas Distribution of Chang 2 Reservoir of Yanchang Formation in Linzhen Area,Ordos Basin[A];[C];2013
4 TANG Jun~(1,2,3),WANG Qi~1,LIAO Peng~(1,2),HAO Le-wei~1,TIAN Bing~(1,2), PANG Guo-yin~(1,2) 1.Key Laboratory of Petroleum Resources Research,Institute of Geology and Geophysics, Chinese Academy of Sciences,Lanzhou 730000,China 2.University of Chinese Academy of Sciences,Beijing,100049,China 3.School of Mathematics,Physics and Biological Engineering,Inner Mongolia University of Science and Technology,Baotou 014010,Inner Mongolia,China;Quantitative simulation of porosity-evolution in the Member 8 sandstone reservoir of the Yanchang formation in Huanxian Oilfield,Ordos Basin[A];[C];2014
5 ZHANG Xiao-li~(1,2),DUAN Yi~1,HE Jin-xian~(1,2),WU Bao-xiang~1,XU Li~1,XIA Jia~1 (1.Key Laboratory of Petroleum Resources Research,Institute of Geology and Geophysics, Chinese Academy of Sciences,Lanzhou 730000,China;2.School of Resource and Earth Science, China University of Mining and Technology,Xuzhou Jiangsu 221008,China);Analysis of Reservoir Forming Conditions of Chang-8 Formation in Huaqing Area,Ordos Basin[A];[C];2014
6 ZHANG Xiao-li~(1,2),DUAN Yi~1,HE Jin-xian~(1,2),WU Bao-xiang~1,XU Li~(1,21),Xia Jia~(1,2) 1.Key Laboratory of Petroleum Resources Research,Institute of Geology and Geophysics,Chinese Academy of Sciences, Lanzhou 730000,China;2.Graduate School of Chinese Academy of Sciences,Beijing 100049,China 3.■■■;Characteristics of the Chang 3 Reservoir in the Yangchang Formation,Linzhen Area,Ordos Basin[A];[C];2014
【Secondary Citations】
Chinese Journal Full-text Database 10 Hits
1 Zhu Guohua (Scientific Research Institute of Petroleum Exploration and Development of Changqing Oil Field);FORMATION OF LOW PERMEABILITY SANDBODIES AND SECONDARY PORE SANDBODIES IN THE UPPER TRIASSIC YANCHANG SERIES OF SOUTH-WESTERN SHAN-CAN-NING BASIN[J];Acta Sedimentologica Sinica;1985-02
2 Mei Zhichao I'm Jinyan (Department of Geology, North an);Stratigraphic Pattern and Character of Skeletal Sand Bodies in Lacustrine Deltas[J];Acta Sedimentologica Sinica;1991-04
3 WEI Hong hong 1 PENG Hui qun 2 LI Jing qun 2 XIE Zheng wen 2 QI Diao liang 2 1 (Department of Geology Northwest University Xi ’an 710069) 2 (Workover Company Changqing Bureau of Petroleum Exploration Qingyang GanSu 745113);Distribution of Sedimentary Facies Belts and Sandstone Bodies of Permo Carboniferous in the Central Part of Ordos Basin[J];ACTA SEDIMENTOLOGICA SINICA;1999-03
4 Li Wenhou 1 Lin Jinyan 1 Yuan Mingsheng 2 and Wang Wuhe 2 1\ (Depatment of Geology, Northwest University, Xi′an\ 710069) 2\ (Research Group of Petroleum Exploration and Development Headquarters in Turpan Hami, Hami\ 73900);Two Types of Coarse Claslic Delta in Turpan Hami Basin[J];ACTA SEDIMENTOLOGICA SINICA;1996-03
5 Liu Shaofeng Ke Airong Wu Liyun and Huang Siji (China University of Geosciences, Wuhan 430074);Sediment Provenance Analysis and Its Tectonic Significance in the Foreland Basin of the Ordos Southwestern Margin[J];ACTA SEDIMENTOLOGICA SINICA;1997-01
6 Lu Zongsheng Huang Qisheng Jiao Yangquan (China University of Geosciences, Wuhan 430074);THE MIDDLE JURASSIC BIVALVE ECOASSEMBLAGE OF YAN'AN FORMATION,NORTHEASTERN ORDOS BASIN,CHINA[J];;1992-03
7 Yue Wenzhe Ye Zhizheng Bi Zhongqi (Nanjing Institute of Geology and Mineral Resources,Nanjing);Sedimentary Environments and Facies Architecture of Middle_Upper Triassic Huangmaqing Formation: A Palaeofluvio_deltaic Depositional System[J];;1999-03
8 YANG Shouye, LI Congxian (Laboratory of Marine Geology, Tongji University, Shanghai 200092,China);RESEARCH PROGRESS IN REE TRACER FOR SEDIMENT SOURCE[J];ADVANCE IN EARTH SCIENCES;1999-02
9 Li Wenhou, Zhou Lifa(Department of Geology , Northwest University, Xi'an, Shaanxi, 710069)Zhao Wenzhi and Xue Liangqin(Scientific Research Institute of Petroleum Exploration and Development, Beijing, 100083);Deltaic Sediments of the Jurassic in Northwestern China[J];Geological Review;1998-01
10 Xue Liangqing and W.E. Galloway (Department of Geological Sciences The University of Texas at Austin, TX 78713, U.S.A.);FAN-DELTA, BRAID DELTA AND THE CLASSIFICATION OF DELTA SYSTEMS[J];Acta Geological Sinica;1991-02
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