Journal of Jilin University(Earth Science Edition) ›› 2016, Vol. 46 ›› Issue (3): 681-691.doi: 10.13278/j.cnki.jjuese.201603106

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Features and Origin of Super-Large Oil Shale Deposit in Southeast Uplift of the Songliao Basin

Wen Zhiliang1, Jiang Fuping1, Zhong Changlin2, Jiang Xuefei1, Wang Guoqian2, Qi Yan1   

  1. 1. Jilin Geological Survey Institute of Jilin Province, Changchun 130061, China;
    2. Geological Archives of Jilin Province, Changchun 130061, China
  • Received:2015-11-20 Online:2016-05-26 Published:2016-05-26
  • Supported by:

    Supported by Special Scientific Research Funds on Public Sectors for the Ministry of Land and Resources(201211051)

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Abstract:

The oil shale deposit is located in the southeast uplift area of Songliao basin, and belongs to a third-class structural unit of Songliao central fault depression in the Jilin-Heilongjiang geosyncline fold system. The studied area was mainly filled with Mesozoic Cretaceous clastic rocks. On the basis of the core observation and "Fischer" oil content test classification, it is concluded that the oil shale developed in dark and brown-black mudstone layers, which mainly distributed in the Qingshankou Formation and the Nenjiang Formation of Cretaceous. The oil shale layers correlation among boreholes and the lateral distribution characteristics show that the oil shale is layered in a large scale, stable distribution, and better continuity. The bulk organic geochemistry data shows the oil yield of oil shale is closely related to organic matter type and total organic carbon content. Meanwhile, oil shale has high ash content, it is low quality oil shale ores. Combining the oil shale features and sedimentary environment, it is concluded that the origin of the oil shale was sapropelic oil shale.

Key words: Songliao basin, southeast uplift, Cretaceous, oil shale deposit, origin of oil shale

CLC Number: 

  • P618.12

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