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《Acta Sedimentologica Sinica》 2009-05
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The Geological Model of Hydrothermal Activity in Outcrop and the Characteristics of Carbonate Hydrothermal Karst of Lower Paleozoic in Tarim Basin

PAN Wen-qing1,2 LIU Yong-fu2 Dickson J A D3 SHEN An-jiang4 HAN Jie2 YE Ying5 GAO Hong-liang2 GUAN Ping1 ZHANG Li-juan2 ZHENG Xing-ping4(1.Peking University,Beijing 100871;2.Institute of Tarim Oilfield Company,PetroChina,Korla,Xingjiang 841000;3.Cambridge University,England;4.Hangzhou Institute of Petroleum Geology,PetroChina,Hangzhou 310023;5.Zhejiang University,Hangzhou 310027)  
Along with the continuously proceeding of petroleum exploration in the Lower Palaeozoic carbonate in Tazhong area,a series of hydrothermal minerals such as fluorite,sphalerite,schatzite,baritite,anhydrite,pyrobitumen,and hydrothermal quartz and their associations are found in the Ordovician reservoir in outcrops and the relative exploration wells of Tazhong area repectively,More and more geological data show that the hydrothermal karst reservoir may be an important type neglected in the Lower Palaeozoic carbonate petroleum exploration in Tarim Basin.By the observation and measurements of outcrop hydrothermal karst phenomena in the recent six years,large amount of thin sections observation,mineral energy spectrum detecting,formation water strontium isotopes analysis,and study about faults nature of the Ordovician reservoir in well field of Tazhong 82 and 24,The active characteristics of the hydrothermal corrosion fluid and its controlling factor on the formation of quality reservoir are in deep study,The hydrothermal karst reservoir geological model is established finally.The results show that the hydrothermal minerals are mainly developed in the associating structural dissolution fractures along faults,corrosional vugs and the faults,they are the main pathway for hydrothermal fluid migration and the important factors controlling the formation of quality reservoir.The hydrothermal corrosion altering reservoir are widely developed in the Ordovican reservoir in the proximity of the strike faults formed in Hercynian in Tazhong area,which can be the petroleum exploration targets of the Upper Ordovician strata along the strike faults in the western part of Tazhong.
【Fund】: 国家科技重大专项(编号L2008ZX05000-004-004);; 中国石油股份公司重大专项(编号:2008E-0703)资助
【CateGory Index】: P618.13
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1 Huang Wenhui~1 Wang Anjia~1 Wan Huan~1 Fan Tailiang~1 Yu Bingsong~2 1 Key Laboratory of Marine Reservoir Evolution and Hydrocarbon Accumulation Mechanism, Ministry of Education,China University of Geosciences(Beijing),Beijing 100083 2 School of Earth Sciences and Resources,China University of Geosciences(Beijing),Beijing 100083;Discussion on characteristics of the Cambrian-Ordovician carbonate rocks reservoirs and origin of dolostones in Tarim Basin[A];[C];2011
2 LIU Ya-lei~1,HUANG Zhi-bin~2,WU Gen-yao~1,LI Yue-jun~1,HU Xiu-fang~3,WEN Lei~1,ZHANG Qiang~1 (1.Institute of Geology and Geophysics,Beijing 100029,China;2.Tarim Oilfield Company,PetroChina,Korla,Xinjiang 841000,China;3. Department of Ocean Science and Engineering,Zhejiang University,Hangzhou,Zhejiang 310058,China);Distribution and Structural Setting of Magmatic Rocks of Middle-Late Permian in Western Tabei Uplift,Tarim Basin[A];[C];2013
3 LI KaiKai,CAI ChunFang,CAI LiuLu,JIANG Lei and XIANG Lei Key Lab of Petroleum Resources Research,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;Origin of sulfides in the Middle and Lower Ordovician carbonates in Tahe oilfield,Tarim Basin[A];[C];2013
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