Volume 26 Issue 2
Apr.  2020
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Article Navigation >  Journal of Geomechanics  > 2020  >  26(2): 271-284
LI Changhai, LI Gang, WANG Shijie, et al., 2020. Permian very low-grade metamorphism and its potential for hydrocarbon generation in the Linxi-Wulanhaote Area, Inner Mongolia, China. Journal of Geomechanics, 26 (2): 271-284. DOI: 10.12090/j.issn.1006-6616.2020.26.02.026
Citation: LI Changhai, LI Gang, WANG Shijie, et al., 2020. Permian very low-grade metamorphism and its potential for hydrocarbon generation in the Linxi-Wulanhaote Area, Inner Mongolia, China. Journal of Geomechanics, 26 (2): 271-284. DOI: 10.12090/j.issn.1006-6616.2020.26.02.026
shu

Permian very low-grade metamorphism and its potential for hydrocarbon generation in the Linxi-Wulanhaote Area, Inner Mongolia, China

doi: 10.12090/j.issn.1006-6616.2020.26.02.026
  • 1.

    College of Earth Sciences, Jilin University, Changchun 130000, Jilin, China

  • 2.

    Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources, Changchun 130000, Jilin, China

  • 3.

    Liaoning Geological Exploration Institute, Dalian 116100, Liaoning, China

More Information
  • Received: 2020-01-02
  • Revised: 2020-02-25
  • Published: 2020-04-01
    Abstract
  • The very low-grade metamorphism has been the focus of research in recent years and has great significance for the study of structural evolution of young orogenic belt and petroleum exploration. The recent studies revealed that the Carboniferous Permian strata in the northeastern part of China mainly underwent very low-grade metamorphism and gradually became a new petroleum exploration layer. This paper launched studies on the illite crystallinity, illite polytype and illite b0 dimension of the Permian System in the Linxi-Wulanhaote Area. The illite crystallinity ranges from 0.175 to 0.47, mainly clustering between 0.25 and 0.35 with an average of 0.30. Illite b0 ranges from 9.0155 to 9.0316 Å, with an average of 9.0249 Å. Illite polytype is predominantly 2M1. Based on the above data, the Permian System in the study area mainly experienced the prehnite-pumpellyite facies very low-grade metamorphism under medium-pressure with metamorphic temperature at 200~370℃, indicating its potential for hydrocarbon generation. Together with the hydrocarbon generation history of the Permian strata and the widespread Cretaceous granites in the study area, the very low-grade metamorphism might occurred during the early-Cretaceous, related to the increase of geothermal gradient caused by the intrusion of granite.

     

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