ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
塔里木盆地塔中西部地区奥陶系岩溶 作用及对油气储层的制约
  
关键词:karstification  main controlling factors  Ordovician  western Tazhong area
基金项目:中国石化集团公司科技部项目(编号P04027)及中国石化海相前瞻性项目(编号YPH08110)
作者单位E-mail
何碧竹 中国地质科学院地质研究所 国土资源部大陆动力学重点实验室中国石化中原油田分公司 勘探开发科学研究院 hebizhu@vip.sina.com 
焦存礼 中国石油化工股份有限公司 石油勘探开发研究院  
贾斌峰 中国石化中原油田分公司 勘探开发科学研究院  
汪功怀 中国石化中原油田分公司 勘探开发科学研究院  
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摘要:
Karstification of Ordovician Strata in Western Tazhong Area of Tarim Basin, Xijiang
      There exist thick marine carbonate strata of varied lithologic characters in the Lower Ordovician-Upper Ordovician Lianglitage Formation of western Tazhong area. Based on data of drill cores, logs and laboratory tests, the authors recognized three types of karstifications in the study area, namely syn-depositional, weathering-crust, and buried ones. The syn-depositional karstification occurs mainly on the platform margin of Later Ordovician Lianglitage Formation, in which atmospheric lithogenic lens are frequently seen but their sizes are not so big. The weathering-crust karstification is developed in central Kartarke uplift. The buried karstification can be divided into three stages and are distributed in areas where faulted structural belts and igneous rocks are well developed. Lithofacies and sedimentary facies, karstification and structural fissures are main factors controlling the develop-ment of Ordovician carbonate reservoirs, which constrain the development of karst reservoir rocks in different layers and positions.
HE Bi-zhu,JIAO Cun-li,JIA Bin-feng,WANG Gong-huai.2009.Karstification of Ordovician Strata in Western Tazhong Area of Tarim Basin, Xijiang[J].Acta Geoscientica Sinica,30(3):395-403.
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