Lithologic Reservoirs ›› 2009, Vol. 21 ›› Issue (1): 22-26.doi: 10.3969/j.issn.1673-8926.2009.01.005

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Study on the main diagenesis of Ma 51 submember in northeastern Jingbian Gas Field

LI Shilin1，LEI Bianjun2，ZHANGWenji2，LI Gao3，LIU Bin4，WANG Xiaorong5   

  1. 1. Chongqing Gas Field， Southwest Oil and Gas Field Company， Chongqing 400000， China； 2. Southwest Petroleum University， Chengdu 610500， China； 3. Stake Key Laboratory of Oil and Gas Reservoir Geology and Exploitation， Southwest Petroleum University， Chengdu 610500， China； 4. Research Institute of Exploration and Development， Jilin Oilfield Company， Songyuan 138000， China； 5. Central Sichuan Oil and Gas Field， Southwest Oil and Gas Field Company， Suining 629000， China
  • Online:2009-03-16 Published:2009-03-16

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Abstract:

The OrdovicianMa 51 reservoir in northeastern Jingbian Gas Field in Ordos Basin is at the top ofweathering crust. The diagenesis is complex because of weathering and denudation in about 130 Ma. Based on the analysis of core and thin slice, it is concluded that the forming of Ma 51 dolomite reservoir is dominated by hypergene karstification, burial dissolution and mineral filling. The favorable diagenesis zones of Ma 51 reservoir are mainly in the midst-central south and west of the study area.

Key words: lithologic reservoir, the third member of Shahejie Formation, West Sag, Liaohe Depression

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