吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (3): 681-691.doi: 10.13278/j.cnki.jjuese.201603106

• 地质与资源 • 上一篇    下一篇

松辽盆地东南隆起超大型油页岩矿床特征及成因

温志良1, 姜福平1, 钟长林2, 姜雪飞1, 王果谦2, 齐岩1   

  1. 1. 吉林省地质调查院, 长春 130061;
    2. 吉林省地质资料馆, 长春 130061
  • 收稿日期:2015-11-20 出版日期:2016-05-26 发布日期:2016-05-26
  • 作者简介:温志良(1956-),男,三级研究员,主要从事油页岩地质方面的研究,E-mail:wen_zhiliang@163.com
  • 基金资助:

    国土资源部公益性行业科研专项(201211051)

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)

摘要:

研究区内已发现的超大型油页岩矿床位于吉黑地槽褶皱系松辽中断陷的一个三级构造单元——松辽盆地东南隆起内。研究区主要发育白垩纪地层,属于陆源碎屑岩沉积。经钻井岩心观察和采用“费舍尔”方法对含油率测试分析表明,油页岩层主要赋存在早白垩世青山口组和晚白垩世嫩江组。含油页岩层系整体为一套厚层的暗色泥页岩和油页岩组合。井间油页岩层对比和油页岩平面展布特征显示,该区油页岩呈层状、规模大、分布范围广、矿层稳定、连续性好。研究证实矿石含油率与有机质组分及总有机碳关系密切,矿石灰分大,属低品质油页岩矿石。通过对油页岩特征及成矿环境分析,认为矿床成因属于腐泥型页岩-油页岩。

关键词: 松辽盆地, 东南隆起, 白垩系, 油页岩矿床, 矿床成因

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

中图分类号: 

  • P618.12

[1] 钱家麟,王剑秋,李述元. 世界油页岩资源利用和发展趋势[J]. 吉林大学学报(地球科学版), 2006, 36(6):877-887. Qian Jialin, Wang Jianqiu, Li Shuyuan. World Oil Shale Utilization and Its Future[J]. Journal of Jilin University(Earth Science Edition), 2006, 36(6):877-887.

[2] 刘招君,董清水,叶松青,等. 中国油页岩资源现状[J]. 吉林大学学报(地球科学版), 2006, 36(5):869-870. Liu Zhaojun, Dong Qingshui, Ye Songqing, et al. The Situation of Oil Shale Resources in China[J]. Journal of Jilin University(Earth Science Edition), 2006, 36(6):869-870.

[3] 温志良, 姜福平, 初红雁, 等. 吉林省油页岩[M]. 长春:吉林科学技术出版社,2013:8-27,116-121. Wen Zhiliang, Jiang Fuping, Chu Hongyan, et al. Oil Shale in Jilin Province[M]. Changchun:Jilin Science and Technology Press, 2013:8-27,116-121.

[4] 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):1286-1296. Liu Zhaojun, Meng Qingtao, Jia Jianliang, et al. Metallogenic Regularity of Oil Shale in Continental Basin:Case Study in the Meso-Cenozoic of Northeast China[J]. Journal of Jilin University(Earth Science Edition), 2012, 42(5):1286-1296.

[5] 贾建亮, 刘招君, Achim Bechtel, et al. 松辽盆地嫩江组油页岩发育控制因素[J]. 地球科学:中国地质大学学报, 2014,39(2):174-186. Jia Jianliang, Liu Zhaojun, Achim Bechtel, et al. Mahor Factors Controlling Formation of Oil Shale in Nenjiang Formation of Songliao Basin[J]. Earth Science:Journal of China University of Geoscience, 2014,39(2):174-186.

[6] Sun Pingchang, Liu Zhaojun, Reinhard Gratzer, et al. Oil Shale and Bulk Geochemical Parameters in the Songliao and Huadian Basins (China):A Grade Classification Aapproach[J]. Oil Shale, 2013, 30(3):402-418.

[7] Sun Pingchang, Liu Zhaojun, Zhen Zhen, et al. Geologic Conditions of Shale Oil and Gas Accumulation in the Southeast Uplift Songliao Basin (Upper Cretaceous, NE China)[J]. Energy Part A, 2015, 37:477-484.

[8] Jia Jianliang, Achim Bechtel, Liu Zhaojun, et al. Oil Shale Formation in the Upper Cretaceous Nenjiang Formation of the Songliao Basin (NE China):Implications from Organic and Inorganic Geochemical Analyses[J]. International Journal of Coal Geology, 2013, 113:11-26.

[9] 张静平, 唐书恒, 吕建伟, 等. 松辽盆地青山口组一段油页岩成矿条件及有利目标区分析[J]. 地学前缘, 2012, 19(1):156-162. Zhang Jingping, Tang Shuheng, Lü Jianwei, et al. Analyses of Forming Condition and Favorable Area of Oil Shale in the 1st Kember of Qingshankou Formation, Songliao Basin[J]. Earth Science Frontiers, 2012, 19(1):156-162.

[10] 徐公愉,方文昌,崔斗烈,等. 吉林省地质志[M]. 北京:地质出版社, 1989:527-573. Xu Gongyu, Fang Wenchang, Cui Doulie, et al. Jilin Geology Records[M]. Beijing:Geological Publishing House, 1989:527-573.

[11] 郭东鑫, 唐书恒, 解慧, 等. 松辽盆地油页岩勘探开发有利区预测[J]. 西安科技大学学报, 2012, 32(1):57-62. Guo Dongxin, Tang Shuheng, Xie Hui, et al. Favorable Areas Prediction for Oil Shale Exploration and Exploitation in Songliao Basin[J]. Journal of Xi'an University of Science and Technology, 2012, 32(1):57-62.

[12] 迟小燕. 松辽盆地上白垩统油页岩特征及沉积环境分析[J]. 石油天然气学报, 2010, 32(4):161-165. Chi Xiaoyan. Characteristics and Sedimentary Environment of Oil Shale in the Upper Cretaceous of Songliao Basin[J]. Journal of Oil and Gas Technology, 2010, 32(4):161-165.

[13] 刘招君, 孙平昌, 贾建亮, 等. 陆相深水环境层序识别标志及成因解释:以松辽盆地青山口组为例[J]. 地学前缘,2011, 18(4):171-180. Liu Zhaojun, Sun Pingchang, Jia Jianliang, et al. Distinguishing Features and Their Genetic Interpretation of Stratigraphic Sequences in Continental Deep Water Setting:A Case from Qingshankou Formation in Songliao Basin[J]. Earth Science Frontiers, 2011,18(4):171-180.

[14] 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.

[1] 陈爱民. 澳大利亚Bonaparte盆地WA-406-P区块油气成藏条件及控制因素[J]. 吉林大学学报(地球科学版), 2018, 48(4): 965-980.
[2] 李向文, 张志国, 王可勇, 孙加鹏, 杨吉波, 杨贺. 大兴安岭北段宝兴沟金矿床成矿流体特征及矿床成因[J]. 吉林大学学报(地球科学版), 2018, 48(4): 1071-1084.
[3] 孙海涛, 钟大康, 李勇, 毛亚昆, 杨宪彰. 超深低孔特低渗砂岩储层的孔隙成因及控制因素——以库车坳陷克深地区巴什基奇克组为例[J]. 吉林大学学报(地球科学版), 2018, 48(3): 693-704.
[4] 马国庆, 孟庆发, 黄大年. 基于重力异常的松辽盆地构造特征识别[J]. 吉林大学学报(地球科学版), 2018, 48(2): 507-516.
[5] 蔡来星, 卢双舫, 肖国林, 王蛟, 吴志强, 郭兴伟, 侯方辉. 论优质源储耦合关系的控藏作用:对比松南致密油与松北致密气成藏条件[J]. 吉林大学学报(地球科学版), 2018, 48(1): 15-28.
[6] 郝立波, 赵昕, 赵玉岩. 辽宁白云金矿床稳定同位素地球化学特征及矿床成因[J]. 吉林大学学报(地球科学版), 2017, 47(2): 442-451.
[7] 鲍新华, 张宇, 李野, 吴永东, 马丹, 周广慧. 松辽盆地增强型地热系统开发选区评价[J]. 吉林大学学报(地球科学版), 2017, 47(2): 564-572.
[8] 高翔, 刘志宏, 聂志阳, 姚勇, 贾卧, 王超, 宋健. 松辽盆地大庆长垣形成时间的厘定及其地质意义[J]. 吉林大学学报(地球科学版), 2017, 47(1): 74-83.
[9] 林承焰, 曹铮, 任丽华, 张昌盛, 范瑞峰, 王叶, 邢新亚, 马晓兰. 松辽盆地南部大情字井向斜区葡萄花油层石油富集规律及成藏模式[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1598-1610.
[10] 王力, 孙丽伟. 山东省寺庄金矿床成矿流体特征[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1697-1710.
[11] 王晰, 段明新, 任云生, 侯召硕, 孙德有, 郝宇杰. 内蒙古额尔古纳地区八大关铜钼矿床流体包裹体特征与成矿时代[J]. 吉林大学学报(地球科学版), 2016, 46(5): 1354-1367.
[12] 刘财, 杨宝俊, 冯晅, 单玄龙, 田有, 刘洋, 鹿琪, 刘才华, 杨冬, 王世煜. 论油气资源的多元勘探[J]. 吉林大学学报(地球科学版), 2016, 46(4): 1208-1220.
[13] 康健, 韦庆海, 周琳, 高研, 张永刚, 高峰. 利用地震台阵观测资料研究大庆地区深部构造[J]. 吉林大学学报(地球科学版), 2016, 46(3): 900-910.
[14] 郭荣涛, 赵习, 刘红光, 石开波, 刘婧, 蒋启财. 兰州盆地下白垩统碎屑岩层序地层序列:祁连山早白垩世隆升的沉积学响应[J]. 吉林大学学报(地球科学版), 2016, 46(2): 321-335.
[15] 曾令高, 张均, 孙腾, 李斌, 朱光辉, 贾子超, 方权, 陈庚户. 峨眉山大火成岩省烂纸厂铁矿床地质特征、成因及其找矿勘查启示[J]. 吉林大学学报(地球科学版), 2016, 46(2): 412-424.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!