吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (4): 970-981.doi: 10.13278/j.cnki.jjuese.20180148

• 地质与资源 • 上一篇    下一篇

中口子盆地侏罗系煤系烃源岩地球化学特征及生烃潜力评价

牛海青1, 韩小锋2, 肖波3, 魏建设2, 张慧元2, 王宝文2   

  1. 1. 西北大学地质学系, 西安 710069;
    2. 中国地质调查局西安地质调查中心, 西安 710054;
    3. 中国石油长庆油田分公司采油五厂, 西安 710200
  • 收稿日期:2018-06-07 出版日期:2019-07-26 发布日期:2019-07-26
  • 作者简介:牛海青(1982-),女,在站博士后,主要从事石油地质研究,E-mail:upc_nhq@163.com
  • 基金资助:
    国家自然科学基金项目(41330315);中国地质调查局地质调查项目(DD20189612,DD20190092)

Evaluation of Hydrocarbon Generation and Geochemical Characteristics of Coal-Measure Source Rocks,Zhongkouzi Basin in Beishan Area

Niu Haiqing1, Han Xiaofeng2, Xiao Bo3, Wei Jianshe2, Zhang Huiyuan2, Wang Baowen2   

  1. 1. Department of Geology, Northwest University, Xi'an 710069, China;
    2. Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, China;
    3. No.5 Recovery Plant, Changqing Oilfield Company, CNPC, Xi'an 710200, China
  • Received:2018-06-07 Online:2019-07-26 Published:2019-07-26
  • Supported by:
    Supported by National Natural Science Foundation of China (41330315) and Geological Survey Project of China Geolo-gical Survey (DD20189612, DD20190092)

摘要: 甘肃-内蒙古交界处的北山盆地群侏罗系是我国西北地区潜在的油气勘探新领域。为加深对该盆地群资源潜力的认识,以有机地球化学分析数据为基础,探讨了其中煤系烃源岩的沉积环境、有机质来源,建立了该烃源岩生烃潜力评价标准。研究结果表明,中口子盆地侏罗系烃源岩干酪根类型以Ⅱ1-Ⅱ2型为主,生烃母质主要是陆生植物,含少量的藻类和水生生物,主要形成于三角洲平原沼泽或湖侵期的间湾湖泊等氧气量适中的弱氧化-弱还原沉积环境。生烃潜量和氢指数是衡量煤系源岩有机质丰度、生烃潜力和生油潜力最有效的指标,根据生烃潜力评价标准:黑帐房凹陷侏罗系暗色泥岩多属于中-差烃源岩,南泉凹陷暗色泥岩生烃潜力级别优于黑帐房凹陷,主要为中-好烃源岩;南泉凹陷炭质泥岩大多数属于中等-好油源岩,煤岩大多属于差油源岩。

关键词: 煤系烃源岩, 地球化学, 生物标志化合物, 生烃潜力, 侏罗系, 中口子盆地

Abstract: The Jurassic system of Beishan basin group at the junction of Gansu and Inner Mongolia is a new potential field for oil and gas exploration in Northwest China. On the basis of systematic sample collection,the characteristics of organic matter and biomarker of the Jurassic source rocks in Zhongkouzi basin were analyzed in detail by means of testing technology and geochemical analysis. The results show that the kerogen type of the Jurassic source rocks in the middle mouth basin is mainly typeⅡ1-Ⅱ2, and the source material of hydrocarbon generation is mainly terrestrial plants, containing a small amount of algae and aquatic organisms. It is mainly formed in a weak oxidation-weak reduction sedimentary environment with moderate oxygen content, such as swamps or transgressive lakes in delta plain. According to the evaluation criteria of hydrocarbon generation potential, most of the Jurassic dark mudstones in Heizhangfang sag belong to the source rocks with poor or medium hydrocarbon generating potential. The hydrocarbon generating potential of the dark mudstones in Nanquan sag is medium or high,better than that in Heizhangfang sag. Based on the analytical data in Zhongkouzi basin and the discussion on sedimentary environment and sources of organic matter, the evaluation criteria for hydrocarbon generation potential of source rocks in coal measures are established. This study can provide a comparative reference for the study of the Jurassic sedimentary paleo-environment and resource potential in Northwest China.

Key words: coal-measure source rocks, geochemistry, biological marker compound, hydrocarbon generation potential, Jurassic, Zhongkouzi basin

中图分类号: 

  • P618.13
[1] 李明杰,郑孟林,曹春潮,等. 北山-阿拉善地区侏罗-白垩纪盆地的叠合演化[J].石油与天然气地质,2004,25(1):54-57. Li Mingjie, Zheng Menglin, Cao Chunchao, et al. Evolution of Superposed Jurassic and Cretaceous Basins in Beishan-Alxa Area[J]. Oil & Gas Geology, 2004, 25(1):54-57.
[2] 陈启林,杨占龙. 泛河西走廊盆地群油气地质特征与勘探前景[J].天然气地球科学,2010,21(2):186-192. Chen Qilin, Yang Zhanlong. Petroleum Geology of Pan-Hexi Corridor Basins and Exploration Prospecting[J]. Natural Gas Geoscience, 2010, 21(2):186-192.
[3] 李相博,完颜容,王琪,等. 甘肃及邻区中小盆地油气地质特征及资源潜力分析[J].兰州大学学报(自然科学版),2006,42(1):18-22. Li Xiangbo, Wan Yanrong, Wang Qi, et al. Charaeteristies of Petroleum Geology Within Middle and Small Basins and Their Resource Potentials in Gansu and Its Adjacent Regions[J]. Journal of Lanzhou University (Natural Seienees), 2006, 42(1):18-22.
[4] 仁和爱,李刚. 北山地区总口子盆地油气勘探方向[J].海洋地质动态,2005,2(4):24-27. Ren Heai, Li Gang. The Hydrocarbon Exploration Direction of Zongkouzi Basin in Beishan Area[J]. Marine Geology Letters, 2005, 2(4):24-27.
[5] 吴少波,白玉宝,杨友运. 北山盆地群侏罗、白垩系沉积体系及其分布、演化[J].西北大学学报(自然科学版),2003,33(6):717-722. Wu Shaobo, Bai Yubao, Yang Youyun. The Jurassic to Cretaceous Sedimentary Systems and Their distribution in the Beishan Basins Group[J]. Journal of Northwest University (Natural Science Edition), 2003, 33(6):717-722.
[6] 张德润. 北山地区地球物理场特征及基底性质[J]. 物探与化探, 2000, 24(2):87-91. Zhang Derun. Characteristics of Geophysical Field and Properties of Basement in Beishan Area[J]. Geophysical and Geochemical Exploration, 2000, 24(2):87-91.
[7] 左国朝,刘义科,李相博. 蒙甘青宁地区侏罗纪开合盆山构造格局及原型盆地沉积特征[J].地质通报,2004,23(3):261-271. Zuo Guochao, Liu Yike, Li Xiangbo. Jurassic Basin Range Tectonic Pattern and Depositional Features of Prototype Basins in the Inner Mongolia-Gansu-Qinghai-Ningxia Region[J]. Geological Bulletin of China, 2004, 23(3):261-271.
[8] 龚全胜,刘明强,梁明宏,等. 北山造山带大地构造相及构造演化[J].西北地质,2003,36(1):11-18. Gong Quansheng, Liu Mingqiang, Liang Minghong, et al. The Tectonic Facies and Tectonic Evolution of Beishan Orogenic Belt, Gansu[J]. Northwestern Geology, 2003, 36(1):11-18.
[9] 吴少波,白玉宝. 北山盆地群侏罗-白垩系生储盖特征及油气远景[J].地质科学,2006,41(1):1-9. Wu Shaobo, Bai Yubao. Jurassic-Cretaceous Source Rock-Reservoir-Cap Associations and Hydrocarbon Potentials in the Beishan Basins[J]. Chinese Journal of Geology, 2006, 41(1):1-9.
[10] 陆相烃源岩地球化学评价方法:SY/T 5735-1995[S].北京:石油工业出版社,1996. The Evaluation Method of Terrestrial Source Rocks:SY/T 5735-1995[S]. Beijing:Petroleum Industry Press, 1996.
[11] 赵国柱. 辽河油田外围盆地元宝山凹陷烃源岩评价[J].新疆石油天然气,2016,12(1):13-18. Zhao Guozhu. Evaluation of Yuan Baoshan Sag Periphery Basin Hydrocarbon Source Rocks in Liaohe Oilfield[J]. Xinjiang Oil and Gas, 2016, 12(1):13-18.
[12] Hunt J M. Petroleum Geochemistry and Geology[M]. 2nd ed. New York:W HFreem and Co Ltd, 1996.
[13] Peters K E,Moldowan J M. The Biomarker Guide:Interpreting Molecular Fossil in Petroleum and Ancient Sediments[M]. Engle-Wood C1iffs:Prentice Ha11, 1993:88.
[14] 王铁冠. 生物标志物地球化学研究[M]. 武汉:中国地质大学出版社, 1990. Wang Tieguan. Approach to Biomarker Geochemistry[M]. Wuhan:China University of Geoscience Press, 1990.
[15] 王杰,张晓宝,陈践发. 苏里格庙气田煤系烃源岩生烃特征评价[J].煤田地质与勘探,2005,33(2):26-29. Wang Jie, Zhang Xiaobao, Chen Jianfa. Evaluation of the Hydrocarbon-Generating Characteristic for Coal-Bearing Hydrocarbon-Source Rocks of Suligemiao Gas Field[J]. Coal Geology & Exploration, 2005, 33(2):26-29.
[16] Didyk B M. Organic Geochemical Indicators of Paleoenvironmental Conditions of Sedimentation[J]. Nature, 1978, 272:16.
[17] 王炳凯,冯乔,田方正,等. 新疆准噶尔盆地南缘二叠系芦草沟组烃源岩生物标志化合物特征及意义[J].地质通报,2017,36(2/3):304-313. Wang Bingkai, Feng Qiao,Tian Fangzheng, et al. The Characteristics and Significance of Biomarker Compounds in the Permian Lucaogou Formation Hydrocarbon Source Rock on the Southern Margin of the Junggar Basin[J]. Geological Bulletin of China, 2017, 36(2/3):304-313.
[18] 黄正吉,李友川. 渤海湾盆地渤中坳陷东营组烃源岩的烃源前景[J].中国海相油气(地质),2002,16(2):118-124. Huang Zhengji, Li Youchuan. Hydrocarbon Source Potential of Dongying Formation in Bozhong Depression, Bohai Bay Basin[J]. China Offshore Oil and Gas(Geology), 2002, 16(2):118-124.
[19] 鲁静,邵龙义,杨敏芳,等. 陆相盆地沼泽体系煤相演化、层序地层与古环境[J].煤炭学报,2014,39(12):2473-2481. Lu Jing, Shao Longyi, Yang Minfang, et al. Coal Facies Evolution, Sequence Stratigraphy and Palaeoenvironment of Swamp in Terrestrial Basin[J]. Journal of China Coal Society, 2014, 39(12):2473-2481.
[20] 曹寅,钱志浩,张渠. 烃源岩评价分析项目的优化组合[J].海相油气地质,2008,13(3):55-62. Cao Yin,Qian Zhihao,Zhang Qu. Assembling and Optimizing Methods for Experimental Analysis Items in Source Rock Evaluation[J]. Marine Origin petroleum Geology, 2008, 13(3):55-62.
[21] 刘德汉,傅家漠,肖贤明,等.煤成烃的成因与评价[J].石油勘探与开发,2005,32(4):137-140. Liu Dehan, Fu Jiamo, Xiao Xianming, et al. Origin and Appraisal of Coal Derived Gas and Oil[J]. Petroleum Exploration and Development, 2005, 32(4):137-140.
[22] 钱铮, 张松航, 梁宏斌, 等. 冀中坳陷东北部石炭-二叠系烃源岩生烃潜力评价[J]. 吉林大学学报(地球科学版), 2015, 45(5):1332-1341. Qian Zheng, Zhang Songhang, Liang Hongbin, et al. Hydrocarbon Evaluation of Carboniferous-Permian Source Rocks in Northeast Jizhong Depression[J]. Journal of Jilin University (Earth Science Edition), 2015, 45(5):1332-1341.
[23] 陈建平,赵长毅,何忠华. 煤系有机质生烃潜力评价标准探讨[J].石油勘探与开发,1997,24(1):1-5. Chen Jianping, Zhao Changyi, He Zhonghua. Criteria for Evaluating the Hydrocarbon Generating Potential of Organic Matter in Coal Measures[J]. Petroleum Exploration and Development, 1997, 24(1):1-5.
[24] Zhang S C, Zhang B, Zhu G, et al. Geochemical Evidence for Coal-Derived Hydrocarbons and Their Charge History in the Dabei Gas Field, Kuqa Thrust Belt, Tarim Basin, NW China[J]. Marine and Petroleum Geology, 2011, 28(7):1364-1375.
[25] 吴志远,彭苏萍,杜文凤. 吐哈盆地十三间房地区煤系烃源岩生烃评价及排烃特征[J].矿业科学学报, 2016, 1(2):103-112. Wu Zhiyuan, Peng Suping, Du Wenfeng. Evaluation of the Hydrocarbon Generation and Hydrocarbon Expulsion Characteristics of Coal-Measure Source Rock in Shisanjianfang Area, Tuha Basin[J]. Journal of Mining Science and Technology, 2016, 1(2):103-112.
[26] 帅燕华,张水昌,陈建平. 煤和煤系泥岩生油能力再评价[J].地球化学,2009,38(6):583-590. Shuai Yanhua, Zhang Shuichang, Chen Jianping. Comparison of the Oil Potential of Coal and Coaly Mudstone[J]. Geochimica, 2009, 38(6):583-590.
[27] 都鹏燕, 高岗, 魏涛, 等. 雅布赖盆地萨尔台凹陷侏罗系新河组有效烃源岩研究[J].吉林大学学报(地球科学版), 2018, 48(1):29-38. Du Pengyan, Gao Gang, Wei Tao, et al. Effective Source Rocks in Jurassic Xinhe Formation in Sartai Sag, Yabrai Basin[J]. Journal of Jilin University (Earth Science Edition), 2018, 48(1):29-38.
[28] 王东良,李欣,李书琴,等. 未成熟-低成熟煤系烃源岩生烃潜力的评价:以塔东北地区为例[J].中国矿业大学学报(自然科学版),2001,30(3):317-320. Wang Dongliang, Li Xin, Li Shuqin, et al. Assessment Standards for Hydrocarbon-Generating Potential of Hydrocarbon Source Rock in Immature to Low-Matured Coal Measures in Northeastern Tarim Basin[J]. Journal of China University of Mining & Technology, 2001, 30(3):317-320.
[29] 陈建平,黄第藩,李晋超,等. 西北侏罗系煤系有机质成烃模式[J]地球化学,1999,28(4):327-339. Chen Jianping, Huang Difan, Li Jinchao, et al. The Petroleum Generation Model for Organic Matter from Jurassic Coal Measure, Northwest China[J]. Geochimica, 1999, 28(4):327-339.
[30] 邓冬云,胡忠奎. 吐哈盆地煤成油气生烃排烃以及组分特征讨论[J].中国石油和化工标准与质量,2013(8):177. Deng Dongyun, Hu Zhongkui. Coal-Derived Oiland Gas Hydrocarbon Generation of Tuha Basin Hydrocarbon Expulsion Components and Features Discussed[J]. China Petroleum and Chemical Standard and Quality, 2013(8):177.
[31] 陈治军,任来义,贺永红,等. 银额盆地哈日凹陷银根组优质烃源岩地球化学特征及其形成环境[J].吉林大学学报(地球科学版), 2017, 47(5):1352-1364. Chen Zhijun, Ren Laiyi, He Yonghong, et al. Geochemical Characteristics and Formation Environment of High-Quality Hydrocarbon Source Rocks of Yingen Formation in Hari Sag, Yingen-Ejinaqi Basin[J]. Journal of Jilin University (Earth Science Edition), 2017, 47(5):1352-1364.
[1] 周翔. 松辽盆地北部营城组火山岩地球化学特征及地质意义[J]. 吉林大学学报(地球科学版), 2019, 49(4): 1001-1014.
[2] 于介禄, 于介江, 杨万志, 张元厚, 郭秀玮. 东天山觉罗塔格带东段早志留世中酸性侵入岩的年代学、地球化学及构造意义[J]. 吉林大学学报(地球科学版), 2019, 49(3): 690-708.
[3] 王春光, 董晓杰, 徐仲元, 任云伟, 王文龙, 陈煜嵩. 内蒙古红山子地区新太古代变质侵入岩年代学及地球化学特征[J]. 吉林大学学报(地球科学版), 2019, 49(3): 709-726.
[4] 单玄龙, 蔡壮, 郝国丽, 邹欣彤, 赵容生. 地球化学温标估算长白山地热系统热储温度[J]. 吉林大学学报(地球科学版), 2019, 49(3): 662-672.
[5] 鲁倩, 孙景贵, 安久海, 韩吉龙, 褚小磊. 吉林敦化松江河地区中生代似斑状花岗岩成因和形成环境:元素、Hf同位素和锆石U-Pb年代学证据[J]. 吉林大学学报(地球科学版), 2019, 49(3): 673-689.
[6] 单承恒, 王政, 史长浩. 基于综合等级划分方法的土地质量地球化学评价——以吉林省乌拉街镇为例[J]. 吉林大学学报(地球科学版), 2019, 49(3): 817-829.
[7] 严克涛, 郭清海, 刘明亮. 西藏搭格架高温热泉中砷的地球化学异常及其存在形态[J]. 吉林大学学报(地球科学版), 2019, 49(2): 548-558.
[8] 张治波, 朱志军, 王文锋, 徐颖, 李丽荣. 滇西兰坪盆地中-新生代蒸发岩元素地球化学特征及其形成环境[J]. 吉林大学学报(地球科学版), 2019, 49(2): 356-379.
[9] 吴永涛, 韩润生. 滇东北矿集区茂租铅锌矿床地球化学特征[J]. 吉林大学学报(地球科学版), 2019, 49(2): 400-413.
[10] 吴志强, 张训华, 赵维娜, 祁江豪, 蔡来星. 南黄海海相油气勘探前景探讨与问题分析[J]. 吉林大学学报(地球科学版), 2019, 49(1): 26-38.
[11] 付焱鑫, 谭思哲, 侯凯文. 南黄海盆地北凹泰州组烃源岩形成条件及资源潜力分析[J]. 吉林大学学报(地球科学版), 2019, 49(1): 230-239.
[12] 梅西, 张训华, 刘健, 王中波, 郭兴伟, 黄湘通. 南黄海3.50 Ma以来海陆环境演变的元素地球化学记录[J]. 吉林大学学报(地球科学版), 2019, 49(1): 74-84.
[13] 肖国林, 蔡来星, 郭兴伟, 董贺平, 庞玉茂. 北黄海盆地东部坳陷勘探突破对我国近海残留“黑色侏罗系”油气勘探的启示[J]. 吉林大学学报(地球科学版), 2019, 49(1): 115-130.
[14] 王修齐, 滕龙, 郑红军, 方朝刚, 张训华. 下扬子丰城-乐平地区二叠系乐平组页岩气潜力综合评价[J]. 吉林大学学报(地球科学版), 2019, 49(1): 248-260.
[15] 殷征欣, 王海峰, 韩金生, 吕修亚, 沈泽中, 陈静, 贺惠忠, 谢安远, 关瑶, 董超. 南海边缘海多金属结核与大洋多金属结核对比[J]. 吉林大学学报(地球科学版), 2019, 49(1): 261-277.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!