J4 ›› 2009, Vol. 39 ›› Issue (4): 669-675.

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Characteristic of Oil Shale and Paleoenvironment of the Bayingebi Formation in the Lower Cretaceous in Yin’e Basin

CHEN Hui-jun1,LIU Zhao-jun1,2, LIU Rong1,2, GUO Wei1,2, XIAO Guo-ping3,WU Yan-bin3, FU Zhan-rong4,SHI Ji-zhong1, HU Xiao-feng1, MENG Qing-tao1   

  1. 1.College of Earth Sciences, Jilin University, Changchun 130061,China;2.Key Lab for Evolution of Past Life and Environment in Northeast Asia, Ministry of Education, Changchun 130026, China;3.Exploration Project Office in Tuha Filed of China Pertroleum| Hami,Xinjiang 839009,China;4.Team 108 of Inner Mongolia Nonferrous Metals Geological Exploration Bureau, Chifeng|Inner Mongolia 024000,China
  • Received:2008-11-14 Online:2009-07-26 Published:2009-07-26

Abstract:

Oil shale in the Lower Cretaceous in the Yin’e basin occurs in the second and third members of the Bayingebi Formation. By using borehole core and analysis data, the physics, quality, geochemistry, organic geochemistry and distribution of the oil shale from Bayingebi Formation have been studied, and the sedimentary environment, yield power of palaolake, tectonic and paleoclimate of the oil shale also have been studied. The study results indicate that the oil shale from Bayingebi Formation is of low oil-bearing rate, middle volatilization and low generate heat. Oil shale may be divided into four oil layers. The main oil layer shale were developed during highstand system tract. The genetic type of the oil shale are sapropelic and humus type of deep lake. The concentration of the oil shale was controlled by tectonic evolution, sedimentary environment, paleoclimate and paleo-topograph.

Key words: Yin’e basin, Bayingebi Formation, oil shale, paleoenvironment

CLC Number: 

  • P618.13
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