Oil & Gas Geology ›› 2002, Vol. 23 ›› Issue (2): 179-182.doi: 10.11743/ogg20020217

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ORDOVICION REEF IN LUNAN-BACHU AREA AND THEIR RESERVOIR CHARACTERISTICS

Hu Minyi1,2, Zhu Zhongde2, He Ping2, Zhang Jun1, Wang Qingchun 2   

  1. 1. China University of Geosciences, Beijing;
    2. Jianghan Petroleum University, Jingzhou, Hubei
  • Received:2002-03-10 Online:2002-06-25 Published:2012-01-16

Abstract:

Ordovicion reef in Lunan-Bachu area of Tarim basin have been discovered recently in Middle Ordovicion Yi Jianfang Formation and Upper Ordovicion Sang Tama Formation.The reef-build-up organism are mainly composed of Calathium,Lithistida,Batostoma and Archaeoscyphia etc.The reef body,small in size and variety in type,is generally made up of reef base,reef core and reef cap.Characterized by low-porosity-low permeability or low porosity-middle permeability based on the analysis of porosity and permeability,rocks of reef reservoir are not good in general,but the porosity of reef base and reef cap is higher than that of reef core.The reservoirs,controlled by sedimentary structure and diagenesis,are mainly in types of fracture and pore-fracture.

Key words: reef, reservoir, Ordovicion system, Tarim

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