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YANG Zhi ming, WANG Qi, SHI Ji an, LI Man ru, WANG Lei. Controls on the Enrichment of Oil Pools in Qingxi Sag,Jiuxi Basin[J]. Acta Sedimentologica Sinica, 2003, 21(4): 695-700.
Citation: YANG Zhi ming, WANG Qi, SHI Ji an, LI Man ru, WANG Lei. Controls on the Enrichment of Oil Pools in Qingxi Sag,Jiuxi Basin[J]. Acta Sedimentologica Sinica, 2003, 21(4): 695-700.

Controls on the Enrichment of Oil Pools in Qingxi Sag,Jiuxi Basin

  • Received Date: 2003-04-30
  • Publish Date: 2003-12-10
  • A series of Cretaceous lacustrine mudstone, shale, dolomitic mudstone and argillaceous dolostone comprises the main source rocks of Qing xi Sag in the study area.During deposition, the Qingxi Sag was a closed to semi-closed rift basin with strong reducing conditions that was favorable for the preservation and transformation of organic matter.In addition, the thickness of the source rock is very great with the ratio of source rock to st rata over 50%, together with mixing organic types, high content of organic carbon (>1%), which all provided the important material basis for oil pool formation.Himalayan tectonic movement formed lots of compressional reverse faults, shears faults and structural fissures, and resulted instrata and st ructure overstacking to provide impetus and space for organic matter maturity, migration and accumulation of petroleum.
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    [4] 陈建平,赵文智,黄第藩,等.酒东、酒西盆地的异同与油气勘探[J]. 石油勘探与开发,1997,24(6): 12~16[Chen Jianping, Zhao Wenzhi, Huang Difan, et al. Comparison between Jiuxi and Jiudong basin and oil & gas exploration[J]. Petroleum Exploration and Development, 1997, 24(6): 12~16]
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  • Received:  2003-04-30
  • Published:  2003-12-10

Controls on the Enrichment of Oil Pools in Qingxi Sag,Jiuxi Basin

Abstract: A series of Cretaceous lacustrine mudstone, shale, dolomitic mudstone and argillaceous dolostone comprises the main source rocks of Qing xi Sag in the study area.During deposition, the Qingxi Sag was a closed to semi-closed rift basin with strong reducing conditions that was favorable for the preservation and transformation of organic matter.In addition, the thickness of the source rock is very great with the ratio of source rock to st rata over 50%, together with mixing organic types, high content of organic carbon (>1%), which all provided the important material basis for oil pool formation.Himalayan tectonic movement formed lots of compressional reverse faults, shears faults and structural fissures, and resulted instrata and st ructure overstacking to provide impetus and space for organic matter maturity, migration and accumulation of petroleum.

YANG Zhi ming, WANG Qi, SHI Ji an, LI Man ru, WANG Lei. Controls on the Enrichment of Oil Pools in Qingxi Sag,Jiuxi Basin[J]. Acta Sedimentologica Sinica, 2003, 21(4): 695-700.
Citation: YANG Zhi ming, WANG Qi, SHI Ji an, LI Man ru, WANG Lei. Controls on the Enrichment of Oil Pools in Qingxi Sag,Jiuxi Basin[J]. Acta Sedimentologica Sinica, 2003, 21(4): 695-700.
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