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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2006  >  28(1): 49-53
Zhao Xin, Shi Jian, Wang Jinpeng, Wang Qi, Lu Longfei, Wang Lei, Wang Youxiao. DETECTION OF ALKYLATED FLUORENONES AND THEIR ORIGIN IN OIL SANDS OF TRIASSIC, THE ORDOS BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2006, 28(1): 49-53. doi: 10.11781/sysydz200601049
Citation: Zhao Xin, Shi Jian, Wang Jinpeng, Wang Qi, Lu Longfei, Wang Lei, Wang Youxiao. DETECTION OF ALKYLATED FLUORENONES AND THEIR ORIGIN IN OIL SANDS OF TRIASSIC, THE ORDOS BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2006, 28(1): 49-53. doi: 10.11781/sysydz200601049
shu

DETECTION OF ALKYLATED FLUORENONES AND THEIR ORIGIN IN OIL SANDS OF TRIASSIC, THE ORDOS BASIN

doi: 10.11781/sysydz200601049
  • 1.

    Key Laboratory of Gas Geochemistry, Lanzhou Institute of Geology, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China

  • 2. School of Earth Science and Land Resources, Chang'an University, Xi'an, shaanxi 710054, China

  • 3. Graduate school of Chinese Academy of Sciences, Beijing 100039, China

  • Received Date: 2005-06-27
  • Rev Recd Date: 2005-11-25
  • Publish Date: 2006-01-28
    Abstract
  • Six oil sand samples were collected from the sandstone reservoirs of Yanchang Formation in the northwestern areas of the Ordos Basin,Northwest China.Oil sand extracts were analyzed by GC-MS.A series of alkylated fluorenones have been detected.They are products of oxidation-reduction reaction of fluorene and benzo-fluorene in reservoir.This process can be considered as the result of that during the time of subaerial exposure in the later diagenetic stage A,the fluorene and benzo-fluorene in oil sand are oxidized to fouow the permeating of meteoric water with bacteria and oxygen under the alkali-diagenetic enviornment and participation of the sialicate in Yanchang Formation.

     

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