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《Geotectonica Et Metallogenia》 2009-01
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Geological Structure and Its Controls on Giant Oil and Gas Fields in Kuqa Depression,Tarim Basin:A Clue from New Shot Seismic Data

HE Dengfa1,ZHOU Xinyuan2,YANG Haijun2,LEI Ganglin2 and MA Yujie2(1.MOE Key Laboratory of Marine Reservoir Evolution and Hydrocarbon Accumulation Mechanism,China University of Geosciences,Beijing 100083,China;2.Tarim Oilfield Company,PetroChina,Korla 841000,Xinjiang,China)  
The Kuqa depression of Tarim basin formed on the pre-Late Permian Paleozoic folded basement and has undergone the evolution of foreland basin in Late Permian to Triassic,extensional sag basin in Jurassic to Paleogene,and rejuvenated foreland basin in Neogene to Quaternary,respectively.The weak intervals in the basement,the Jurassic coal beds,and the gypsum and salt or mud intervals of Paleogene Kumgrim Formation in the west and the Neogene Jidik Formation in the east have contributed as a whole to detaching shallowly upward from the north to the south.The detachment and the surface which dips shallowly basin-ward,constitute a typical tectonic wedge.The internal structure of the thrust wedge is characterized by the stratification in vertical,zonation horizontally,and segmentation in longitude.The N-W trending Awat-Karayuergun fault and the N-E trending Kuqa fault divide the Kuqa depression into three segments as Wushi sag,Baicheng sag,and Yangxia sag from west to east.The characters of structural layers have controlled largely the regional development of the effective source rocks in Triassic to Jurassic and the occurrence of reservoir-cap rock associations.The structural deformation with a stratification character has decided upon the formation of sub-salt imbricate structures with the thrust faults as the pathways for oil and gas.The combination of fault-related folds and the accordingly imbricate structures have resulted in the occurrence of such composite oil and gas zones or plays.For example,each fault-related folds in the Dabei-Kelasu structural belts has accumulated oil and gas separately,and then they combined together to form a larger composite gas plays.This kind of phenomenon has at present been proven partly by the Dabei gas play,the sub-Kelasu gas play and the Kelasu gas play.The tear faults or the transfer faults have controlled the enrichment in oil and gas in different blocks or segments.The Kuqa depression is a favorable area for oil and gas to accumulate.Thus,it is a promising area for petroleum exploration.However,the geological structures have played a great role in the zonation of different types of oil and gas fields in the area at present.
【Fund】: 国家重点基础研究发展计划(编号:2006CB202300);; 国家自然科学重点基金(编号:40739906)资助
【CateGory Index】: P618.13
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5 Chen Chuming 1\ Lu Huafu 1\ Jia Dong 1\ Xie Xiaoan 2 1(Dept of Earth Sciences, Nanjing University, Nanjing\ 210093) 2(Bureau of Geophysical Prospecting, CNPC\ Zuozhou Hebei\ 072751);Neogene Quaternary Sedimentary Features,Structural Deformation of the Tarim Basin and its Petroleum Geological Significances[J];ACTA SEDIMENTOLOGICA SINICA;1998-02
6 JIA Dong;LU Huafu;CAI Dongsheng;CHEN Chuming (Department of Earth Sciences, Nanjing University, Nanjing 210093);STRUCTURAL ANALYSES OF KUQA FORELAND FOLD-THRUST BELT ALONG THE NORTHERN MARGIN OF TARIM BASIN[J];GEOTECTONICA ET METALLOGENIA;1997-01
7 ZHANG Zhong pei, LIN Wei and WANG Qing chen(Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China);PROGRESSIVE STRUCTURAL EVOLUTION OF KELASU-YIQIKELIKE STRUCTURAL BELT IN KUQA DEPRESSION[J];Geotectonica Et Metallogenia;2003-04
8 XU Zhengyu1, LI Dacheng1, LU Wenzhong1, LIN Ge2 and LIU Chiyang3 (1. Hangzhou Institute of Petroleum Geology, PetroChina Company Limited, Hangz hou 310023, China; 2. Guangzhou Institute of Geochemistry, Chinese Academy of Sc iences, Guangzhou 510640, China; 3. Department of Geology, Northwest University, Xi’an 710069, China);PATTERN ANALYSES AND GENETIC INTERPRETATION ABOUT THE GEOTECTONICS OF YUDONG (EAST CHONGQING)[J];Geotectonica Et Metallogenia;2004-01
9 WU Shimin, ZHOU Di and LIU Hailing (Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanolo gy &Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510301, China);TECTONIC FRAMEWORK AND EVOLUTIONARY CHARACTERISTICS OF NANSHA BLOCK,SOUTH CHI NA SEA[J];Geotectonica Et Metallogenia;2004-01
10 ZHANG Minqiang~1, ZHONG Zhihong~1, XIA Bin~1, LI Xuxuan~1, SUN Zhen~2, WANG Liangshu~3 and Wang Zhenfeng~4 (1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, GD 510640, China; 2. South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, GD 510301, China; 3. The Department of Earth Sciences, Nanjing University, Nanjing, JS 210093, China; 4. Nanhai West Corporation, CNOOC, Zhanjiang, GD 524057, China);GENETIC MECHANISMS OF MUD-FLUID DIAPIR IN YINGGEHAI BASIN AND HYDROCARBON ACCUMULATION[J];Geotectonica Et Metallogenia;2004-02
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