Journal of Jilin University(Earth Science Edition) ›› 2020, Vol. 50 ›› Issue (2): 378-391.doi: 10.13278/j.cnki.jjuese.20190247

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Controlling Factors of Oil Shale and Coal Oil Yield in Lower Cretaceous Muling Formation in Laoheishan Basin

Song Yu1,2, Liu Zhaojun2,3, Achim Bechtel4, Xu Yinbo5, Meng Qingtao2,3, Sun Pingchang2,3, Zhu Kai1   

  1. 1. Key Laboratory of Tectonics and Petroleum Resources(China University of Geosciences), Ministry of Education, Wuhan 430074, China;
    2. Key Laboratory of Oil Shale and Coexistent Energy Minerals of Jilin Province, Changchun 130061, China;
    3. College of Earth Sciences, Jilin Universiry, Changchun 130061, China;
    4. Department of Applied Geosciences and Geophysics, Montanuniversitaet Leoben, Leoben A-8700, Austria;
    5. Oil&Gas Survey Center, China Geological Survey, Beijing 100083, China
  • Received:2019-11-23 Online:2020-03-26 Published:2020-03-31
  • Supported by:
    Supported by National Natural Science Foundation of China (41902139) and Open Fund of Key Laboratory of Oil Shale and Coexistent Energy Minerals of Jilin Province (DBY-ZZ-18-04)

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Abstract: The paragenetic oil shale and coal are widely developed in continental basins of China. The authors took the oil shale and coal of the lower Cretaceous Muling Formation in Laoheishan basin as a study object, and studied the controlling factors of oil yield of oil shale and coal, combined with both industrial parameters (oil yield, ash content, volatile matter, total sulfur, and gross calorific value) and organic geochemical analyses (total organic carbon, Rock-Eval, maceral, and biomarker analyses). The oil shale and coal are classified into four types, including high oil yield oil shale (HOS), low oil yield oil shale (LOS), high oil yield coal (HC), and low oil yield coal (LC). The highest TOC and S1+S2 values are observed in HC, followed by LC, HOS, and LOS, all types are of type Ⅱ kerogen and in immature stage. The source of organic matter and depositional environment are the key controlling factors of oil yield in oil shale and coal. HC was deposited in mire with abundant input of terrestrial organic matter; in contrast, HOS was formed in limnology environment with moderate input of terrestrial organic matter. The floral assemblage is characterized by the presence of Pinaceae, Cupressaceae/Taxodiaceae, Araucariaceae, Podocarpaceae and ferns during the formation of oil shale and coal. These plants could provide abundant resinous and waxy organic matter, which lead to relatively high oil yield of oil shale and coal.

Key words: Laoheishan basin, Lower Cretaceous, oil shale and coal, oil yield, ornigac geochemistry

CLC Number: 

  • P618.12
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