Lithologic Reservoirs ›› 2008, Vol. 20 ›› Issue (4): 33-37.doi: 10.3969/j.issn.1673-8926.2008.04.006

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Diagenesis and porosity evolution of deep volcanic reservoirs in Songliao Basin

LIU Chenglin1，DU Yunhua2，GAO Jiayu2，JIN Hui2，LIU Renhe2，FAN Bojiang1，ZHU Yuxin3，ZHU Jie1   

  1. 1. State Key Laboratory of Petroleum Resources and Prospecting， China University of Petroleum， Beijing 102249， China； 2. Research Institute of Petroleum Exploration & Development-Langfang， PetroChina， Langfang 065007， China； 3. Research Institute of Petroleum Exploration & Development， PetroChina， Beijing 100083， China
  • Online:2008-12-15 Published:2008-12-15

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Abstract:

Based on core description, thin section analysis, pore character and microphotograph, the diagenesis and pore evolution of deep volcanic reservoirs in Songliao Basin are studied. It is believed that the rock types are mainly basalt, andesite, rhyolite, tuff and volcanic breccia. The reservoir spaces include primary pore, primary fracture, secondary pore and secondary fracture. The diagenesis and the pore evolution could be divided into two stages （eruption stage and post-eruption stage） which include condensation phase, thermogenesis phase, hypergenesis phase and burial diagenesis phase. The reservoir spaces are affected by the diagenesis events including metasomatism, faulting, pressure solution, deep denudation and hydrocarbon aggregation.

Key words: pore structure, reservoir evaluation, Lower Karamay Formation, Junggar Basin

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