Journal of Jilin University(Earth Science Edition) ›› 2020, Vol. 50 ›› Issue (2): 392-404.doi: 10.13278/j.cnki.jjuese.20190265

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Geochemical Characteristics and Paleolimnological Information of Oil Shale in 1st Member of Qingshankou Formation in Northern Songliao Basin

Zheng Guodong1,2, Meng Qingtao3,4, Liu Zhaojun3,4   

  1. 1. Lunan Geological Engineering Investigation Institute of Shandong Province, Jining 272100, Shandong, China;
    2. Engineering Innovation Center for Restoration&Reclamation in Mining-Induced Subsidence Land of MNR, Jining 272100, Shandong, China;
    3. College of Earth Sciences, Jilin University, Changchun 130061, China;
    4. Key Laboratory of Oil Shale and Coexistent Energy Minerals of Jilin Province, Changchun 130061, China
  • Received:2019-12-09 Online:2020-03-26 Published:2020-03-31
  • Supported by:
    Supported by National Natural Science Foundation of China (41872103) and Project of China Geological Survey (1212011220800)

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Abstract: The geochemical characteristics and paleolimnological information of oil shale are the key evidence to reveal the rule of metallogeny and enrichment of oil shale. Based on the analyses of TOC, oil yield, rock pyrolysis, element, biomarker compound,and organic maceral, geochemical characteristics of oil shale in the 1st Member of Qingshankou Formation in Well ZY1 in northern Songliao basin the were refinedly characterized, paleolimnological information recorded by the oil shale was analyzed, then the control effect of paleolake on organic matter enrichment of oil shale was discussed. The results show that there are 8 layers of medium-high quality oil shale in the 1st Member of Qingshankou Formation, and the high quality oil shale is mainly in the lower part. The TOC of oil shale has good correlation with the oil yield. Seen from the thermal evolution, the oil shale is in the immature-low mature stage with high hydrocarbon potential. Abundant steranes and terpanes are detected from the oil shale samples. The organic matter type of oil shale is mainly Ⅰ, and the main source of organic matter is lake aquatic organisms dominated by lamalginite. The paleolacustrine productivity of the lower part can be divided into three cycles by geochemical parameters, correspondingly the water salinity of paleolake shows three cycles from semi-saline to saline, and the redox property of paleo-lake shows reduction-strong reduction-reduction. And the paleolacustrine productivity of the late cycle Ⅱ is the highest, corresponding to the highest water salinity and the strongest reducibility. It is suggested that the high lake yield caused by lake eutrophication is the material basis of organic matter enrichment of high-quality oil shale in the 1st Member of Qingshankou Formation, and the strong reduction environment of bottom water controlled by salinity stratification is favorable for the accumulation of organic matter in high-quality oil shale.

Key words: oil shale, geochemical, paleolimnology, 1st Member of Qingshankou Formation, Songliao basin

CLC Number: 

  • P618.12
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