Journal of Jilin University(Earth Science Edition) ›› 2020, Vol. 50 ›› Issue (2): 326-340.doi: 10.13278/j.cnki.jjuese.20190312

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Oil Shale Features and Sedimentary Environment in Jianchang Basin, Western Liaoning Province

Wang Simin1,2, Zang Dongsheng1,2, Wang Xiqiong3, Li Jie1,2, Han Song1,2, Li Jianzhong1,2   

  1. 1. State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum(Beijing), Beijing 102249, China;
    2. College of Geosciences, China University of Petroleum(Beijing), Beijing 102249, China;
    3. Exploration&Development Research Institute of Liaohe Oilfield, Panjin 124010, Liaoning, China
  • Received:2019-12-27 Online:2020-03-26 Published:2020-03-31
  • Supported by:
    Supported by National Science and Technology Major Project (2017ZX05032-001-001) and Cooperation and Innovation Research Projects of National Potential Oil and Gas Resources (Exploration, Development and Utilization of Oil Shale) (OSR-01-11)

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Abstract: Jianchang basin, located in western Liaoning Province, is rich in oil shale resources. Based on the data of outcrops, drilling and laboratory analyses, distribution and petrological characteristics, the geochemical characteristics and sedimentary environment of oil shale were analyzed. The study shows that the oil shale is in the first, second and third members of Jiufotang Formation, totally nine ore groups. The average oil content and thickness of the third member of Jiufotang Formation are better than those of others. The average oil content of the oil shale is 5.15%, the average ash content is 81.9%, the total sulfur content is low, and the average calorific value is 5.19 kJ/g, belonging to medium-high calorific oil shale. The technically identified recoverable resources of oil shale and shale oil are 8.22×108 t and 3.17×107 t respectively in the area of Jianchang, Wujiazi, Jiufotang, Qidaoquanzi, and Daqingshan. It is predicted that there is 9.27×1010 t oil shale resources in Jianchang basin. There are abundant organic matter in immature-low mature stage, mainly type Ⅰ and type Ⅱ1. During Jiufotang Formation, the climate was warm and humid, a large quantity of organic matter from land and lakes were deposited, and the sedimentary environment was in the state of freshwater and brackish reduction, which was conducive to the preservation of organic matter.

Key words: oil shale, biomarker, sedimentary environment, Jiufotang Formation, Jianchang basin

CLC Number: 

  • P618.12
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