吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (4): 1090-1099.doi: 10.13278/j.cnki.jjuese.201604110
刘招君1,2, 孙平昌1,2, 柳蓉1,2, 孟庆涛1,2, 胡菲1,2
Liu Zhaojun1,2, Sun Pingchang1,2, Liu Rong1,2, Meng Qingtao1,2, Hu Fei1,2
摘要:
古近纪敦密断裂带上分布一系列的含油页岩盆地群。根据盆地间构造-沉积充填、岩石组合和油页岩赋存特征,初步确认盆地群中油页岩沉积于湖盆鼎盛阶段,均形成于古近系始新统路特阶。盆地群间油页岩矿床特征存在明显的差别,由西南向东北,油页岩厚度逐渐变小,其沉积环境由深湖到半深湖,再到湖沼,而有机质来源则由湖泊生物为主,到湖泊生物和陆源有机质双向来源,过渡为以陆源高等植物为主。结合含油页岩层系形成于同一时期和相似的古气候背景下,盆地沉降和沉积充填作用是影响油页岩矿床差异的关键因素。长期处于欠补偿环境,可容纳空间大的湖盆利于巨厚油页岩的形成,随着可容纳空间的减少、陆源碎屑供给的增多,油页岩厚度减薄,分布也变得相对局限。深湖和湖沼成因油页岩品质较好,半深湖油页岩品质较差。
中图分类号:
[1] 吴根耀,马力,梁兴,等. 从郯庐断裂带两侧的"盆""山"耦合演化看前白垩纪"郯庐断裂带"的性质[J]. 地质学报,2008,27(3):308-325. Wu Genyao, Ma Li, Liang Xing, et al. The Nature of the Pre-Cretaceous "Tanlu Fault Zone" Viewed in the Light of Basin Range Coupling Evolution on Its Both Sides[J]. Geological Bulletin of China, 2008, 27(3): 308-325.[2] 陈荣度. 从辽宁东、西部地质对比论郯庐断裂的平移运动[J]. 辽宁地质, 1995, 9: 184-193. Chen Rongdu. On the Translation Movement of Tan-Lu Fracture From Geological Correlation Between East and West Liaoning[J]. Liaoning Geology, 1995, 9:184-193.[3] 张贻侠,孙运生,张兴洲,等.中国满洲里绥芬河地学断面[M]. 北京:地质出版社, 1999:15-56. Zhang Yixia, Sun Yunsheng, Zhang Xingzhou, et al. Manzhouli-Suifenhe Global Geoscience Transect (GCT) of North China[M]. Beijing: Geological Publishing House, 1999:15-56.[4] 孙晓猛,王书琴,王英德,等. 郯庐断裂带北段构造特征及构造演化序列[J]. 岩石学报,2010, 26(1):165-176. Sun Xiaomeng, Wang Shuqin, Wang Yingde, et al. The Structural Feature and Evolutionary Series in the Northern Segment of Tancheng-Lujiang Fault Zone[J]. Acta Petrologica Sinica, 2010, 26(1):165-176.[5] 刘志宏,梅梅,高军义,等. 东北东部虎林盆地的构造特征、成盆机制及敦密断裂带北东段的形成时代[J]. 吉林大学学报(地球科学版),2014,44(2):480-489. Liu Zhihong, Mei Mei, Gao Junyi, et al. Strctural Features, Formation Mechanism of Hulin Basin and Deformation Time of Northeastern Segment of Dunhua-Mishan Fault Zone in Northeast China[J]. Journal of Jilin Unversity: Earth Science Edition, 2014, 44(2): 480-489.[6] Quan C, Liu Y S C, Utescher T. Paleogene Temperature Gradient, Seasonal Variation and Climate Evolution of Northeast China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2012, (313/314): 150-161.[7] 胡善亭, 康西栋, 吴克平, 等.梅河盆地聚煤环境分析[J].中国煤田地质, 1996, 8(2): 13-15. Hu Shanting, Kang Xidong, Wu Keping, et al. Sedimentary Coal Accumulating Environment of Meihe Basin[J]. Coal Geology of China, 1996, 8(2): 13-15.[8] 张普林,吕宝臣,李春田,等. 早第三纪桦甸动物群的发现及其地质意义[J]. 吉林地质,1986,4:1-11. Zhang Pulin, Lü Baochen, Li Chuntian, et al. Discovery of the Huadian Fauna of the Early Tertiary and Its Geological Significance[J]. Jilin Geology, 1986, 4: 1-11.[9] 孟庆涛. 桦甸盆地始新统油页岩岩石地球化学特征及富集规律研究[D]. 长春:吉林大学,2010: 27-53. Meng Qingtao. Research on Petrologic and Geochemical Characteristics of Eocene Oil Shale and Its Enrichment Regularity, Huadian Basin[D]. Changchun: Jilin University, 2010:27-53.[10] 王海峰,张廷山,戴传瑞,等. 敦化盆地上侏罗统上新统地层划分对比讨论[J].中国地质,2008,35(1):40-53. Wang Haifeng, Zhang Tingshan, Dai Chuanrui, et al. Stratigraphic Division and Correlation of the Upper Jurassic-Pliocene in the Dunhua Basin[J]. Geology in China, 2008, 35(1): 40-53.[11] 王东方.抚顺古新世玄武岩特征及其在郯庐断裂发展中的构造意义[J].岩石矿物学杂志,1986,5(3):212-219. Wang Dongfang. The Paleocene Basalt in Fushun District and Their Tectonic Significance in Development of Tancheng-Lujiang Fault Belt[J]. Acta Petrologica et Mineralogica, 1986, 5(3): 212-219.[12] 景建安,王宁,黎伟. 宁安盆地构造演化与找铀矿远景预测[J]. 铀矿地质,2008,24(3):143-149. Jing Jian'an, Wang Ning, Li Wei. The Structural Evolution and Prognosis of Uranium Exploration in Ning'an Basin[J]. Uranium Geology, 2008, 24(3): 143-149.[13] 王珊. 鸡西盆地早白垩世城子河组穆棱组沉积体系分析[D]. 武汉:中国地质大学,2012:9-14. Wang Shan. Depositional System Analysis of Early Cretaceous Chengzihe-Muling Formation in Jixi Basin Northeastern China[D]. Wuhan: China University of Geosciences, 2012: 9-14.[14] 谭宝德. 虎林盆地七虎林河坳陷下第三系虎林组烃源岩地球化学特征[J]. 内蒙古石油化工,2011,12:132-135. Tan Baode. The Geochemical Characteristics of Hydrocarbon Source Rocks of Qihulin River Depress in HuLin Basin[J]. Inner Mongolia Petrochemical Industry, 2011, 12: 132-135.[15] 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, Yan Hulin, Dong Qingshui, et al. Oli Shale in China[M].Beijing: Petroleum Industry Press, 2009: 38-116.[16] Bai Y Y, Liu Z J, Sun P C, et al. Rare Earth and Major Element Geochemistry of Eocene Fine-grained Sediments in Oil Shale-and Coal-Bearing Layers of the Meihe Basin, Northeast China[J]. Journal of Asian Earth Sciences, 2015, 97: 89-101.[17] 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):47-50. Liu Rong, Liu Zhaojun, Liu Feng, et al. High Grade and Low Grade Oil Shale Metallogenic Mechanism of Eocene Jijuntun Formation in Funshun Basin[J]. Petroleum Geology & Oilfield Development in Daqing, 2008, 27(2): 47-50.[18] Strobl S A I, Sachsenhofer R F, Bechtel A, et al. Depositional Environment of Oil Shale Within the Eocene Jijuntun Formation in the Fushun Basin (NE China)[J]. Marine and Petroleum Geology, 2014, 56: 166-183.[19] 徐银波,柳蓉,刘招君,等. 梅河盆地古近纪梅河组有机质富集规律及沉积演化研究[J]. 煤炭学报,2013,38(11):2007-2016. Xu Yinbo, Liu Rong, Liu Zhaojun, et al.Deposition and Enrichment Pattern of Organic Matter of the Meihe Formation in the Paleogene,Meihe Basin[J].Journal of China Coal Society, 2013, 38 ( 11) : 2007-2016.[20] 李宝毅,姚树青,孙平昌,等. 梅河盆地油页岩特征及成因[J]. 世界地质,2014,33 ( 2 ) : 457-464. Li Baoyi,Yao Shuqing, Sun Pingchang, et al. Characteristics and Origin of Oil Shale in Meihe Basin[J]. Global Geology, 2014, 33(2) : 457-464.[21] Sun P C, Sachsenhofer R F, Liu Z J, et al. Organic Matter Accumulation in the Oil Shale-and Coal-Bearing Huadian Basin (Eocene; NE China)[J]. International Journal of Coal Geology, 2013, 105: 1-15.[22] 孙平昌, 刘招君, 孟庆涛, 等. 桦甸盆地古近纪充填特征及对油页岩成矿的影响[J]. 煤炭学报, 2011, 36(7): 1110-1116. Sun Pingchang, Liu Zhaojun, Meng Qingtao, et al. Effect of the Basin-Fill Features on Oil Shale Formation in Paleogene, Huadian Basin[J]. Journal of China Coal Society, 2011, 36(7): 1110-1116.[23] Strobl S A I, Sachsenhofer R F, Bechtel A, et al. Deposition of Coal and Oil Shale in NE China: The Eocene Huadian Basin Compared to the Coeval Fushun Basin[J]. Marine and Petroleum Geology, 2015, 64: 347-362.[24] 郭文秀,温志良,刘建民,等. 吉林省油页岩[M]. 长春:吉林科学技术出版社,2013:116-145. Guo Wenxiu, Wen Zhiliang, Liu Jianmin, et al. Oil Shale Deposits in Jilin Province[M]. Changchun: Jilin Science and Technology Publishing House, 2013: 116-145.[25] 于明德,王璞珺,蒋永福,等. 敦化盆地烃源岩地球化学特征及其生烃潜力[J]. 石油实验地质,2008,30( 3) : 270-275. Yu Mingde, Wang Pujun, Jiang Yongfu, et al. Geochemical Characteritics of Source Rocks and Its Hydrocarbon Generation Potential in the Dunhua Basin[J]. Petroleum Geology & Experiment, 2008, 30( 3) : 270-275.[26] 朱峰. 柳树河盆地和宁安盆地油页岩成藏环境研究[D]. 北京:中国地质大学,2010:9-30. Zhu Feng. Environment Studies of Oil Shale in Liushuhe and Ning'an Basin[D]. Beijing: China University of Geosciences, 2010: 9-30.[27] 周动力,董青松. 黑龙江宁安盆地古近系油页岩沉积环境分析[J]. 东北石油大学学报,2014,38(1):25-30. Zhou Dongli, Dong Qingsong. Analysis of Sedimentary Environment of Palaeogene Oil Shale in Heilongjiang Ning'an Basin[J]. Journal of Northeast Petroleum University, 2014, 38(1): 25-30.[28] 柏静儒,韩冰,李梦迪,等. 黑龙江鸡西油页岩综合利用过程能效分析[J]. 东北电力大学学报,2015,35(4):56-61. Bai Jingru, Han Bing, Li Mengdi, et al. Energy Efficiency Analysis of Heilongjiang Jixi Oil Shale Compressive Utilization[J]. Journal of Northeast Dianli University, 2015, 35(4): 56-61.[29] 姜翠莹. 虎林盆地油页岩沉积特征[J]. 煤炭技术,2009,28(11):132-133. Jiang Cuiying. Oil Shale Sedimentary Features of Hulin Basin[J]. Coal Technology, 2009, 28(11): 132-133.[30] 张晓畅. 虎林盆地虎1井烃源岩评价及油源对比[J]. 大庆师范学院学报,2012,32(3):110-112. Zhang Xiaochang. Source Rock Evaluation and Oil-Source Correlation of Hu1Well in Hulin Basin[J]. Journal of Daqing Normal University, 2012, 32(3): 110-112.[31] Carroll A R, Bohacs K M. Stratigraphic Classification of Ancient Lakes: Balancing Tectonic and Climatic Controls[J]. Geology, 1999, 27: 99-102. |
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