Journal of Jilin University(Earth Science Edition) ›› 2020, Vol. 50 ›› Issue (2): 313-325.doi: 10.13278/j.cnki.jjuese.20200017

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Oil Shale Characteristics and Distribution in Typical Basins of China

Liu Zhaojun1,2, Liu Rong1,2, Sun Pingchang1,2, Meng Qingtao1,2, Hu Fei1,2   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Key Laboratory of Oil Shale and Coexistent Energy Minerals of Jilin Province, Changchun 130061, China
  • Received:2020-01-15 Online:2020-03-26 Published:2020-03-31
  • Supported by:
    Supported by Key Science and Technology Research and Development Project of Jilin Province (20180201077SF)

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Abstract: The characteristics of oil shale deposits in continental basins in China are wildly distributed. Taking Songliao basin,Fushun and Huadian Basin in the Dunmi fault zone,Junggar basin, and Ordos basin as examples,the authors analyzed four types of basins:discrete continental rift basin,transitional strike slip basin,convergent foreland basin, and intraplate craton basin,and summarized oil shale characteristics and their distribution. Among them,the oil shale of discrete continental rift basin deposited in the post rift thermal subsidence evolution stage has the characteristics of organic matter type Ⅰ,medium oil yield,stable thickness, and wide distribution area,which is easy to form super large oil shale deposits, while the oil shale of discrete continental rift basin deposited in the same rift has the characteristics of organic matter type Ⅱ1-Ⅱ2, medium oil yield, medium thickness, and small distribution area, which is easy to form medium oil shale deposits; the oil shale in the conversion strike slip basin has the characteristics of Ⅱ1-Ⅱ2 organic matter and medium-small overall distribution range, but the occurrence of deposits is quite different depending on the extent of the structural subsidence of the strike slip movement fault depression, which tends to form not only oil shale deposits with medium oil yield and huge thickness, but also oil shale deposits with high oil yield and thin thickness; the oil shale deposited in the continental molasse stage of convergent foreland basin has the characteristics of Ⅰ-Ⅱ1 types of organic matter, high oil yield, large thickness, but limited distribution and large changes in stratigraphic occurrence, which is easy to form large oil shale deposits; the oil shale deposited in the stage of intracontinental depression of craton basin has the characteristics of Ⅰ-Ⅱ1 types of organic matter, medium oil yield, stable thickness, and wide distribution area, which is easy to form super large oil shale deposits. Among all types of basins,deep lake environment, high system tract, and transgressive system tract are favorable for oil shale formation.

Key words: characteristics and distribution of oil shale, discrete continental rift basin, transitional strike slip basin, convergent foreland basin, intraplate craton basin

CLC Number: 

  • P631.12
[1] Qian J L, Yin L. Oil Shale-Petroleum Alternative[M]. Beijing:China Petrochemical Press,2011:1-50.
[2] Brendow K. Global Oil Shale Issues and Perspectives[J]. Oil Shale,2003,20(1):81-92.
[3] Hilger J. Combined Utilization of Oil Shale Energy and Oil Shale Minerals Within the Production of Cement and Other Hydraulic Binders[J]. Oil Shale, 2003,20(3):347-355.
[4] Hou J L, Ma Y, Li S Y, et al. Development and Utilization of Oil Shale Worldwide[J]. Chemical Industry and Engineering Progress, 2015, 34(5):1183-1190.
[5] An B C, Wang W Y, Ji G J, et al. Preparation of Nano-Sized α-Al2O3 from oil Shale Ash[J]. Energy, 2010, 35(1):45-49.
[6] Zhang Z K, Zhang L, Li A M. Remedial Processing of Oil Shale Sly Ash (OSFA) and Its Value-Added Conversion into Glass-Ceramics[J]. Waste Manage,2015,46:316-321.
[7] Vallner L, Gavrilova O, Vilu R. Environmental Risks and Problems of the Optimal Management of an Oil Shale Semi-Coke and Ash Landfill in Kohtla-Järve, Estonia[J]. Sci Total Environ, 2015, 524/525:400-415.
[8] Dyni J R. Geology and Resources of Some World Oil-Shale Deposits[J]. Oil Shale, 2003, 20(3):193-252.
[9] 刘招君,杨虎林,董清水,等.中国油页岩[M].北京:石油工业出版社,2009:38-116. Liu Zhaojun, Yang Hulin, Dong Qingshui, et al. Oil Shale in China[M]. Beijing:Petroleum Industry Press,2009:38-116.
[10] 柳蓉,刘招君.国内外油页岩资源现状及综合开发潜力分析[J]. 吉林大学学报(地球科学版),2006,36(6):892-898. Liu Rong,Liu Zhaojun. Analysis on the Current Situation and Comprehensive Development Potential of Oil Shale Resources at Home and Abroad[J]. Journal of Jilin University (Earth Science Edition), 2006,36(6):892-898.
[11] 刘招君,孟庆涛,柳蓉,等.中国陆相油页岩特征及成因类型[J].古地理学报,2009,11(1):105-114. Liu Zhaojun,Meng Qingtao,Liu Rong,et al.Characteristics and Genetic Types of Continental Oil Shale in China[J]. Journal of Palaeogeography,2009,11(1):105-114.
[12] 刘招君, 孟庆涛, 贾建亮,等. 陆相盆地油页岩成矿规律:以东北地区中、新生代典型盆地为例[J]. 吉林大学学报(地球科学版), 2012, 42(5):1286-1297. Liu Zhaojun,Meng Qingtao,Jia Jianliang,et al. Metallogenic Regularity of Oil Shale in Continental Basin:Case Study in the Meso-Cenozoic Basins of Northeast China[J]. Journal of Jilin University (Earth Science Edition), 2012, 42(5):1286-1297.
[13] 刘招君,孙平昌,柳蓉,等. 中国陆相盆地油页岩成因类型及矿床特征[J]. 古地理学报,2016,18(4):525-534. Liu Zhaojun,Sun Pingchang,Liu Rong, et al. Genetic Types and Deposit Features of Oil Shale in Continental Basin in China[J]. Journal of Palaeogeography,2016,18(4):525-534.
[14] 刘招君,孙平昌,柳蓉,等.敦密断裂带盆地群油页岩特征及成矿差异分析[J].吉林大学学报(地球科学版),2016,46(4):1090-1099. Liu Zhaojun,Sun Pingchang,Liu Rong,et al. Research on Oil Shale Features and Metallogenic Differences in Dunhua-Mishan Fault Zone Basins[J]. Journal of Jilin University(Earth Science Edition), 2016,46(4):1090-1099.
[15] 柳蓉. 东北地区东部新生代断陷盆地油页岩特征及成矿机制研究[D].长春:吉林大学,2007. Liu Rong. Research on Shale Characteristics and Metallogenic Mechanism of Cenozoic Fault Basins in Eastern Northeast Region[D]. Changchun:Jilin University,2007.
[16] 柳蓉,刘招君,刘沣,等.抚顺盆地始新世计军屯组油页岩贫富矿成矿机制[J].大庆石油地质与开发,2008,27(2):47-49. Liu Rong,Liu Zhaojun,Liu Feng,et al. Metallogenic Mechanism of the Oil Shale Poor and Rich in the Eocene Jijuntun Formation, Fushun Basin[J]. Petroleum Geology & Oilfield Development in Daqing,2008,27(2):47-49.
[17] 柳蓉,刘招君,杜江峰,等.依兰盆地始新统达连河组油页岩成因新认识[J]. 吉林大学学报(地球科学版),2012,42(4):941-947. Liu Rong,Liu Zhaojun,Du Jiangfeng,et al. New Understanding of the Genesis of the Oil Shale of the Eocene Dalianhe Formation in the Yilan Basin[J]. Journal of Jilin University(Earth Science Edition), 2012, 42(4):941-947.
[18] 柳蓉,刘招君,柳世友,等.依兰盆地油页岩与煤赋存特征及成矿规律研究[J]. 煤炭学报,2012,37(5):776-781. Liu Rong,Liu Zhaojun,Liu Shiyou,et al. Study on Occurrence Characteristics and Metallogenic Regularity of Oil Shale and Coal in Yilan Basin[J]. Journal of China Coal Society, 2012,37(5):776-781.
[19] Sun Pingchang,Liu Zhaojun,Bai Yueyue,et al. Geologic Conditions of Shale Oil and Gas Accumulation in the Southeast Uplift Songliao Basin (Upper Cretaceous,NE China)[J]. Energy Sources,2015,37(5):477-484.
[20] Ingersoll R V, Busby C J. Tectonics of Sedimentary Basins[M]. Oxford:Blackwell,1995:221-262.
[21] 刘招君, 王东坡, 刘立,等. 松辽盆地白垩纪沉积特征[J]. 地质学报,1992,66(4):327-338. Liu Zhaojun,Wang Dongpo,Liu Li,et al. Sedimentary Characteristics of the Cretaceous Songliao Basin[J]. Acta Geologica Sinica, 1992,66(4):327-338.
[22] 陈书平,张一伟,汤良杰.准噶尔晚石炭世-二叠纪前陆盆地的演化[J].石油大学学报(自然科学版),2001,25(5):26-30,38,6. Chen Shuping,Zhang Yiwei,Tang Liangjie. Evolution of the Late Carboniferous-Permian Boreland Basin in Junggar[J]. Journal of University of Petroleum(Edition of Natural Science),2001,25(5):26-30,38,6.
[23] 李勇,王成善,伊海生.中生代羌塘前陆盆地充填序列及演化过程[J].地层学杂志,2002,26(1):62-67. Li Yong,Wang Chengshan,Yi Haisheng. Filling Sequence and Evolution of Qiangtang Foreland Basin in Mesozoic[J]. Journal of Stratigraphy,2002,26(1):62-67.
[24] 张峰,王辉,刘池洋.羌塘盆地中生代构造属性[J].中国煤炭地质,2010,22(4):1-5. Zhang Feng,Wang Hui,Liu Chiyang. Mesozoic Tectonic Attributes in the Qiangtang Basin[J].Coal Geology of China, 2010,22(4):1-5.
[25] 任纪舜,王作勋,陈炳蔚,等.从全球看中国大地构造:中国及邻区大地构造图简要说明[M].北京:地质出版社,2005. Ren Jishun,Wang Zuoxun,Chen Bingwei,et al. A Global View of China's Geotectonics:A Brief Explanation of China and Its Neighboring Geotectonics[M]. Beijing:Geological Publishing House,2005.
[26] 刘招君,胡菲,孙平昌,等. 再论陆相三级层序内四分方案及其在油气勘探中的应用[J].吉林大学学报(地球科学版), 2013, 43(1):1-12. Liu Zhaojun,Hu Fei,Sun Pingchang,et al. Re-Discussion on the Four Division Scheme About Continental Sequence Stratigraphy and Its Application in Oil and Gas Exploration[J]. Journal of Jilin University (Earth Science Edition), 2013, 43(1):1-12.
[27] Feng Zihui,Fang Wei,Wang Xue, et al. Microfossils and Molecular Records in Oil Shales of the Songliao Basin and Implications for Paleo-Depositional Environment[J]. Science in China Series D:Earth Sciences, 2009, 52(10):1559-1571.
[28] Feng Zhiqiang, Jia Chengzao, Xie Xinong, et al. Tectonostratigraphic Units and Stratigraphic Sequences of the Nonmarine Songliao Basin, Northeast China[J]. Basin Research, 2010, 22(1):79-95.
[29] 柳蓉. 东北地区东部新生代断陷盆地油页岩特征及成矿机制研究[D].长春:吉林大学,2007. Liu Rong. Research on Shale Characteristics and Metallogenic Mechanism of Cenozoic Fault Basins in Eastern Northeast Region[D]. Changchun:Jilin University,2007.
[30] 张明明. 基于生物地球化学的博格达山北麓二叠系芦草沟组含油页岩系中有机质聚集模型的建立[D].长春:吉林大学,2016. Zhang Mingming. Establishment of Organic Matter Aggregation Models in the Oil Shale Bearing Series of Permian Lucaogou Formation in the Northern Bogeda Mountain Based on Biogeochemistry[D]. Changchun:Jilin University,2016.
[31] 张坤. 鄂尔多斯盆地南缘三叠系延长组长7油页岩段有机质富集特征[D].长春:吉林大学,2018. Zhang Kun. Enrichment Characteristics of Organic Matter in the Chang 7 Oil Shale Section in Triassic Yanchang Formation in Southern Margin of Ordos Basin[D]. Changchun:Jilin University,2018.
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