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Geoscience ›› 2023, Vol. 37 ›› Issue (05): 1321-1335.DOI: 10.19657/j.geoscience.1000-8527.2023.005

• Petroleum Geology • Previous Articles     Next Articles

Kinetic and Hydrocarbon Generation of Middle Permian Black Shale Around the Bogda Mountain, Southern Junggar Basin: Implications for Petroleum Exploration

JIN Xiao1,2,3(), FENG Yanfang1,2, LUO Xiaoling1,2, WEN Xinyu4, ZHANG Suowen5, ZHANG Zhihuan3   

  1. 1. Development and Research Center, China Geological Survey, Beijing 100037, China
    2. Command Center of Natural Resource Comprehensive Survey, Beijing 100055, China
    3. China University of Petroleum (Beijing), Beijing 102249, China
    4. China Ordins Group Company, Beijing 100089, China
    5. Daqing Oilfield of CNPC, Daqing, Heilongjiang 163002, China
  • Received:2022-05-28 Revised:2023-02-27 Online:2023-10-10 Published:2023-11-14

Abstract:

To explore the hydrocarbon potential of Middle Permian organic-rich mudstone around the Bogda Mountain, the hydrocarbon generation kinetics were studied in different tectonic units.Furthermore, we discussed the physicochemical significance of kinetic results from different methods and the chemical mechanism affecting activation energy.The results show that: controlled by heating temperature, the isothermal hydrous pyrolysis was mainly focused on the oil generation from kerogen, while Rock-Eval experiments show bulk hydrocarbon generation from the source rocks; major peaks of hydrocarbon generation activation energy of source rocks are ~55 kcal/mol (northeast of Bogda Mountain), ~60 kcal/mol (Quanzijie section, northern Bogda Mountain), and 65 to 70 kcal/mol (Jingjingzigou and Chaiwobu); activation energy required for alkane cyclization (higher than that of other dehydrogenation) may be the driving force of high pyrolysis activation energy of type-I organic matter, with abundant alkane components; large-scale hydrocarbon accumulation may have occurred in deep strata under thrust faults.

Key words: hydrocarbon generation kinetics, Lucaogou Formation, Bogda Mountain, organic-rich shale, burial history

CLC Number: