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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2009  >  31(3): 270-274
Liu Xianfeng, Cai Zhongxian, Yun Lu, Xu Wei. ELEMENT GEOCHEMISTRY CHARACTERISTIC RESPONSE FOR KARSTIFICATION IN THE TAHE OILFIELD[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2009, 31(3): 270-274. doi: 10.11781/sysydz200903270
Citation: Liu Xianfeng, Cai Zhongxian, Yun Lu, Xu Wei. ELEMENT GEOCHEMISTRY CHARACTERISTIC RESPONSE FOR KARSTIFICATION IN THE TAHE OILFIELD[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2009, 31(3): 270-274. doi: 10.11781/sysydz200903270
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ELEMENT GEOCHEMISTRY CHARACTERISTIC RESPONSE FOR KARSTIFICATION IN THE TAHE OILFIELD

doi: 10.11781/sysydz200903270
  • 1.

    China University of Geosciences, Faculty of Resources, Wuhan, Hubei 430074, China

  • 2. China University of Geosciences, Graduate School, Wuhan, Hubei 430074, China

  • 3. China University of Geosciences, Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, Wuhan, Hubei 430074, China

  • 4. Design and Planning Institute of Northwest Petroleum Bureau, SINOPEC, Urumqi, Xinjiang 830011, China

  • 5. Exploration Research Dept.CNOOC Research, Beijing 100027, China

  • Received Date: 2008-03-16
  • Rev Recd Date: 2009-04-02
  • Publish Date: 2009-06-28
    Abstract
  • The Tahe Oilfield is located in the southwest margin of Akekule Uplift in north Tarim Basin.It went through several times tectonic uplift from the late Caledonian to the early Hercynian,this lead to Ordovician carbonate formation be exposed to the surface for a long time and suffering from intense air fresh-water weathering,leaching and dissolving and developed a set of complicated superficial karst system.Throuth research of arenaceous and pelitic karstic cave deposit about its' trace element such as B,V,Ga,Rb,etc,and REE characteristic in the main region of the Tahe Oilfield,it indicated that most samples took on characteristic of fresh-water corrosion.While,samples of the four wells such as T615 showed influenced by seawater,it can be indicated that seawater-freshwater mixing corrosion caused by widely marine transgression in early of Carboniferous Period probably overlay and improved the Ordovician karst system in the Tehe Oilfield.

     

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