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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2019  >  41(3): 427-434
WANG Ping, XIANG Liange, JIANG Haijian, CHEN Qingtang, SHI Dahai, CHEN Qianglu, WANG Jie, XU Liangfa. Cretaceous oil-source correlation in Guaizihu Sag, Yin'gen-E'ji'naqi Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2019, 41(3): 427-434. doi: 10.11781/sysydz201903427
Citation: WANG Ping, XIANG Liange, JIANG Haijian, CHEN Qingtang, SHI Dahai, CHEN Qianglu, WANG Jie, XU Liangfa. Cretaceous oil-source correlation in Guaizihu Sag, Yin'gen-E'ji'naqi Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2019, 41(3): 427-434. doi: 10.11781/sysydz201903427
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Cretaceous oil-source correlation in Guaizihu Sag, Yin'gen-E'ji'naqi Basin

doi: 10.11781/sysydz201903427

  • 1. Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, China;

  • 2. Geological Survey Institute of Ningxia Hui Autonomous Region, Yinchuan, Ningxia 750021, China;

  • 3. Zhongyuan Oil Field Branch Company, SINOPEC, Puyang, Henan 457000, China

  • Received Date: 2018-08-15
  • Rev Recd Date: 2019-03-18
  • Publish Date: 2019-05-28
    Abstract
  • Recently, high oil product was gained in the second member of the Cretaceous Bayingebi Formation (K1b2) in the well X in the Guaizihu Sag of Yin'gen-E'ji'naqi Basin, which revealed a bright exploration prospect. It has not obtained a quite unified understanding of petroleum source, so some research were made on the oil-source correlation,which will be helpful for the prediction of hydrocarbon reservoir and the selection of exploration direction. The analyses of composition, biomarker and carbon isotope were made with oil sand samples from the first member of Suhongtu Formation (K1s1), crude oil samples from the second member of Bayingebi Formation, and mudstone samples from the second member of Suhongtu Formation (K1s2) as well as and the second and first members of Bayingebi Formation. The geochemical features of oil sands, crude oil are close with K1b1 source rocks, showing high contents of C30-diahopane and gammacerane, low Pr/Ph and high maturity. The good similarity reflects that K1s1 oil sands and K1b2oil are homologous, and their parent material are both from K1b1source rocks.

     

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