吉林大学学报(地球科学版) ›› 2017, Vol. 47 ›› Issue (5): 1352-1364.doi: 10.13278/j.cnki.jjuese.201705103

• 地质与资源 • 上一篇    下一篇

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

陈治军, 任来义, 贺永红, 刘护创, 宋健   

  1. 陕西延长石油(集团)有限责任公司研究院, 西安 710075
  • 收稿日期:2016-12-07 出版日期:2017-09-26 发布日期:2017-09-26
  • 作者简介:陈治军(1980),男,高级工程师,主要从事石油地质学方面的研究,E-mail:chenzhijun2203@aliyun.com
  • 基金资助:
    国家自然科学基金项目(41202104);陕西延长石油(集团)有限责任公司科技攻关项目(ycsy2016ky-A-09)

Geochemical Characteristics and Formation Environment of High-Quality Hydrocarbon Source Rocks of Yingen Formation in Hari Sag,Yingen-Ejinaqi Basin

Chen Zhijun, Ren Laiyi, He Yonghong, Liu Huchuang, Song Jian   

  1. Research Institute of Yanchang Petroleum(Group) Co. Ltd, Xi'an 710075, China
  • Received:2016-12-07 Online:2017-09-26 Published:2017-09-26
  • Supported by:
    Supported by National Natural Science Foundation of China (41202104) and Science and Technology Project of Shaanxi Yangchang Petroleum (Group) Co., Ltd. (ycsy2016ky-A-09)

摘要: 对于低勘探程度盆地,寻找优质烃源岩对于勘探方向的选择具有重要意义。本文基于大量测试分析资料,以哈日凹陷为研究对象,对银额盆地银根组优质烃源岩的岩石学和地球化学特征进行了研究,并对该烃源岩中有机质来源及其形成环境进行了分析。研究表明,优质烃源岩岩性为泥晶白云岩和白云质泥岩。烃源岩w(TOC)平均5.62%,有机质丰度极高;有机质类型为Ⅰ—Ⅱ1型,属腐泥型,或腐殖腐泥型有机质;烃源岩成熟度较低,但底部已经达到成熟热演化阶段,具有较高的生烃潜力。优质烃源岩的有机质来自高等植物和水生生物的混合源。优质烃源岩Pr/Ph值为0.19~0.27,代表强还原性的沉积环境;伽马蜡烷指数为0.30~0.54,高伽马蜡烷含量表明高盐度的沉积环境。藻类勃发形成的高生产力和缺氧环境是银根组优质烃源岩形成的2个关键条件。

关键词: 银额盆地, 哈日凹陷, 银根组, 优质烃源岩, 地球化学特征, 形成环境

Abstract: For a basin with low degree exploration, looking for the high-quality hydrocarbon source rocks is significant for the choice of exploration direction. Based on a large amount of test and analysis data, we took Hari sag in Yingen-Ejinaqi basin as the research object, and studied the petrological and geochemical characteristics of the high-quality source rocks in Yingen Formation, the source of organic matter, and their forming conditions. The results reveal that the source rocks are micritic dolomites and dolomitic mudstones. The average value of w(TOC) of the source rock is 5.62%, extremely high abundance of organic matters. The organic matter is type I-type Ⅱ1, belonging to sapropel, or partial sapropel. Although the overall maturity is relatively low, the bottom of the source rocks has reached the mature thermal evolution stage with high potential of hydrocarbon generation. The source of organic matter is the mixed of higher plants and aquatic organisms. The Pr/Ph value of high quality source rocks is 0.19-0.27, which represents a strong reducing sedimentary environment; the gammacerane index is 0.30-0.54, and such high content of gammacerane shows its high salinity of sedimentary environment. High productivity generated by algae blooming and anoxic environment are the two key conditions to form high-quality hydrocarbon source rocks.

Key words: Yingen-Ejinaqi basin, Hari sag, Yingen Formation, high-quality hydrocarbon source rocks, geochemical characteristics, formation environment

中图分类号: 

  • TE121.3
[1] 卢双舫, 马延伶, 曹瑞成, 等. 优质烃源岩评价标准及其应用:以海拉尔盆地乌尔逊凹陷为例[J]. 地球科学:中国地质大学学报, 2012, 37(3):535-544. Lu Shuangfang, Ma Yanling, Cao Ruicheng,et al. Evaluation Criteria of High Quality Source Rocks and Its Applications:Taking the Wuerxun Sag in Hailaer Basin as an Example[J]. Earth Science:Jouranl of China University of Geoscience, 2012, 37(3):535-544.
[2] 张林晔, 孔祥星, 张春荣, 等. 济阳坳陷下第三系优质烃源岩的发育及其意义[J]. 地球化学, 2003, 32(1):35-42. Zhang Linye, Kong Xiangxing, Zhang Chunrong, et al. High-Quality Oil-Prone Source Rocks in Jiyang Depression[J]. Geochimica, 2003, 32(1):35-42.
[3] 侯读杰, 张善文, 肖建新, 等. 济阳坳陷优质烃源岩特征与隐蔽油气藏的关系分析[J]. 地学前缘, 2008, 15(2):137-146. Hou Dujie, Zhang Shanwen, Xiao Jianxin,et al. The Excellent Source Rocks and Accumulation of Stratigraphic and Lithologic Traps in the Jiyang Depression, Bohai Basin[J]. Earth Science Frontiers, 2008, 15(2):137-146.
[4] 张文正, 杨华, 傅锁堂, 等. 鄂尔多斯盆地长91湖相优质烃源岩的发育机制探讨[J]. 中国科学D辑:地球科学, 2007, 37(增刊Ⅰ):33-38. Zhang Wenzheng, Yang Hua, Fu Suotang, et al. Discussion on Development Mechanism of Chang 91 Lacustrine High-Quality Hydrocarbon Source Rocks in Ordos Basin[J]. Science in China Press, 2007, 37(Sup.Ⅰ):33-38.
[5] 朱光有, 金强. 东营凹陷两套优质烃源岩地质地球化学特征研究[J]. 沉积学报, 2003, 21(3):506-512. Zhu Guangyou, Jin Qiang. Geochemical Characteristics of Two Sets of Excellent Source Rocks in Dongying Depression[J]. Acta Sedimentologica Sinica, 2003, 21(3):506-512.
[6] 李天义, 何生, 杨智. 海相优质烃源岩形成环境及其控制因素分析[J]. 地质科技情报, 2008, 27(6):63-71. Li Tianyi, He Sheng, Yang Zhi. The Marine Source Rock Formation Conditions and Control Factors[J]. Geological Science and Technology Information, 2008, 27(6):63-71.
[7] 王铁冠. 试论我国某些原油与生油岩中的沉积环境标志物[J]. 地球化学, 1990, 19(3):256-262. Wang Tieguan. A Contribution to Some Sedimentary Environmental Biomarkers in Crude Oils and Source Rocks in China[J]. Geochimica, 1990, 19(3):256-262.
[8] 陈践发, 张水昌, 孙省利, 等. 海相碳酸盐岩优质烃源岩发育的主要影响因素[J]. 地质学报, 2006, 80(3):467-473. Chen Jianfa, Zhang Shuichang, Sun Shengli, et al. Main Factors Influencing Marine Carbonate Source Rock Formation[J]. Acta Geologica Sinica, 2006, 80(3):467-473.
[9] 张文正, 杨华, 杨奕华, 等. 鄂尔多斯盆地长7优质烃源岩的岩石学、元素地球化学特征及发育环境[J]. 地球化学, 2008, 37(1):59-64. Zhang Wenzheng, Yang Hua, Yang Yihua, et al. Petrology and Element Geochemistry and Development Environment of Yanchang Formation Chang-7 High Quality Source Rocks in Ordos Basin[J]. Geochimica, 2008, 37(1):59-64.
[10] 刘新颖, 邓宏文, 邸永香, 等. 海拉尔盆地乌尔逊凹陷南屯组优质烃源岩发育特征[J]. 石油实验地质, 2009, 31(1):68-73. Liu Xinying, Deng Hongwen, Di Yongxiang,et al. High Quality Source Rocks of Nantun Formation in Wuerxun Depression, the Hailaer Basin[J]. Petroleum Geology & Experiment, 2009, 31(1):68-73.
[11] 田春桃, 马素萍, 杨燕, 等. 湖相与海相碳酸盐岩烃源岩生烃条件对比[J]. 石油与天然气地质, 2014, 35(3):336-341. Tian Chuntao, Ma Suping, Yang Yan, et al. Comparison of Hydrocarbon Generation Conditions Between Lacustrine and Marine Carbonate Source Rocks[J]. Oil & Gas Geology, 2014, 35(3):336-341.
[12] 初广震, 张矿明, 柳佳期. 湖相碳酸盐岩油气资源分析与勘探前景[J]. 资源与产业, 2010, 12(2):99-102. Chu Guangzhen, Zhang Kuangming, Liu Jiaqi. Analysis and Prospects of Oil-Gas Resources in Lacustrine Carbonate Rocks[J]. Resources & Industries, 2010, 12(2):99-102.
[13] Freytet P, Verrecchia E P. Lacustrine and Palustrine Carbonate Petrography:An Overview[J]. Journal of Paleolimnology, 2002, 27(2):221-237.
[14] 王力, 金强, 林腊梅, 等. 柴达木盆地西部古近系-新近系优质烃源岩特征[J]. 天然气工业, 2009, 29(2):23-26. Wang Li, Jin Qiang, Lin Lamei, et al. Characteristics of Quality Tertiary Source Rocks in West Qaidam Basin[J]. Natural Gas Industry, 2009, 29(2):23-26.
[15] 刘春燕, 林畅松, 吴茂炳, 等. 银根-额济纳旗中生代盆地构造演化及油气勘探前景[J]. 中国地质, 2006, 33(6):1328-1335. Liu Chunyan, Lin Changsong, Wu Maobing,et al. Tectonic Evolution and Petroleum Prospects of the Mesozoic Yinggen-Ejinaqi Basin, Inner Mongolia[J]. Geology in China, 2006, 33(6):1328-1335.
[16] 刘鑫金, 冯阵东, 李聪, 等. 近源湖盆砂砾岩储层次生溶孔成因探讨:以查干凹陷祥6井区为例[J]. 吉林大学学报(地球科学版), 2017, 47(2):393-404. Liu Xinjin, Feng Zhendong, Li Cong, et al. Discussion of Secondary Pore Origin in Near Source Sandy Conlomerate Reservoir:A Case Study of Xiang 6 Well Area in Chagan Depression[J]. Journal of Jilin University (Earth Science Edition), 2017, 47(2):393-404.
[17] 钟福平, 钟建华, 王毅, 等. 银根-额济纳旗盆地苏红图坳陷早白垩世火山岩地球化学特征与成因[J]. 矿物学报, 2014, 34(1):107-116. Zhong Fuping, Zhong Jianhua, Wang Yi,et al. Geochemistry Characteristics and Origin of Early Cretaceous Volcanic Rocks in Suhongtu Depression, Inner Mongolia, China[J]. Acta Mieralogica Sinica, 2014, 34(1):107-116.
[18] 张代生. 银根-额济纳旗盆地油气地质条件与勘探方向[J]. 吐哈油气, 2002, 7(1):5-10. Zhong Daisheng. The Oil and Gas Geologic Condutions and Exploration Potential of Yingen-Ejinaqi Basin[J]. Tuha Oil & Gas, 2002, 7(1):5-10.
[19] 岩石中可溶有机物及原油族组分分析 SYT5119-2008[S]. 北京:石油工业出版社, 2008. Analysis Method for Fractions of Rock Extract and Crude Oil SYT5119-2008[S]. Beijing:Petroleum Industry Press, 2008.
[20] 陆相烃源岩地球化学评价方法 SYT 5735-1995[S]. 北京:石油工业出版社, 1995. Evaluation Criteria for Organic Matter of Terrestrial Hydrocarbon Source Rock SYT 5735-1995[S]. Beijing:Petroleum Industry Press, 1995.
[21] 卢双舫, 张敏. 油气地球化学[M]. 北京:石油工业出版社, 2010:206-213. Lu Shuangfang, Zhang Min. Oil and Gas Geochemical[M]. Beijing:Petroleum Industry Press, 2010:206-213.
[22] 杜治利, 田亚, 刘洪军, 等. 鄂尔多斯盆地南部延长组长9段页岩气资源潜力评价[J]. 吉林大学学报(地球科学版), 2016, 46(2):358-367. Du Zhili, Tian Ya, Liu Hongjun, et al. Shale Gas Resource Potential Evalution of Chang 9 Member, Yanchang Formation in South Ordos Basin[J]. Journal of Jilin University (Earth Science Edition), 2016, 46(2):358-367
[23] 孙耀庭, 徐守余, 张世奇, 等. 山东昌乐凹陷油页岩地球化学特征及成因探讨[J]. 吉林大学学报(地球科学版), 2015, 45(3):736-742. Sun Yaoting, Xu Shouyu, Zhang Shiqi, et al. Geochemical Characteristics and Genesis of the Oil Shale in Changle Sag, Shandong Province[J]. Journal of Jilin University (Earth Science Edition), 2015, 45(3):736-742.
[24] 邬立言, 顾信章. 热解技术在我国生油岩研究中的应用[J]. 石油学报, 1986, 7(2):13-19. Wu Liyan, Gu Xinzhang. The Application of Pyrolysis Technique in Source Rock Research[J]. Acta Petrolei Sinica, 1986, 7(2):13-19.
[25] 侯读杰, 张林晔. 实用油气地球化学图鉴[M]. 北京:石油工业出版社, 2003. Hou Dujie, Zhang Linye. Practical Oil and Gas Geochemical Map[M]. Beijing:Petroleum Industry Press, 2003.
[26] 王香增, 贺永红, 张立宽, 等. 鄂尔多斯盆地吴起-志丹地区长10烃源岩特征与生烃潜力[J]. 天然气地球科学, 2013, 24(3):461-469. Wang Xiangzeng, He Yonghong, Zhang Likuan,et al. Geochemical Characteristics and Hydrocarbon Generation Potentials of Chang 10 Source Rock in Wuqi-Zhidan Area, Ordos Basin[J]. Natural Gas Geoscience, 2013, 24(3):461-469.
[27] 柳广弟. 石油地质学[M]. 北京:石油工业出版社, 2010:153-170. Liu Guangdi. Petroleum Geology[M]. Beijing:Petroleum Industry Press, 2010:153-170.
[28] 杜治利, 曾昌民, 邱海峻, 等. 塔西南叶城凹陷二叠系两套烃源岩特征及柯东1井油源分析[J]. 吉林大学学报(地球科学版), 2016, 46(3):651-660. Du Zhili, Zeng Changmin, Qiu Haijun, et al. Key Formations of the Permian Hydrocarbon Source Rocks and Oil-Source Correlation of Well KD1 in Yecheng Depression of Southwestern Tarim Basin[J]. Journal of Jilin University (Earth Science Edition), 2016, 46(3):651-660.
[29] 任拥军, 杜雨佳, 郭潇潇, 等. 渤中凹陷古近系优质烃源岩特征及分布[J]. 油气地质与采收率, 2015, 22(1):5-13. Ren Yongjun, Du Yujia, Guo Xiaoxiao, et al. Characteristics and Distribution of Paleogene High-Quality Source Rocks in Bozhong Sag[J]. Petroleum Geology and Recovery Efficiency, 2015, 22(1):5-13.
[30] 侯读杰, 冯子辉. 油气地球化学[M]. 北京:石油工业出版社, 2011:205-243. Hou Dujie, Feng Zihui. Oil and Gas Geochemical[M]. Beijing:Petroleum Industry Press, 2011:205-243.
[31] 张立平, 黄第藩, 廖志勤. 伽马蜡烷:水体分层的地球化学标志[J]. 沉积学报, 1999, 17(1):136-140. Zhang Liping, Huang Difan, Liao Zhiqin. Gammacerane:Geochemical Indicator of Water Column Stratification[J]. Sedimentologica Sinica, 1999, 17(1):136-140.
[32] 孙钰, 钟建华, 袁向春, 等. 国内湖相碳酸盐岩研究的回顾与展望[J]. 特种油气藏, 2008, 15(5):1-6. Sun Yu, Zhong Jianhua, Yuan Xiangchun, et al. Review and Prospect of the Study on Domestic Lacustrine Carbonate Rocks[J]. Special Oil & Gas Reservoirs, 2008, 15(5):1-6.
[33] 周自立, 杜韫华. 湖相碳酸盐岩的沉积相与油气分布关系:以山东胜利油田下第三系碳酸盐岩为例[J]. 石油实验地质, 1986, 17(2):123-132. Zhou Zili, Du Yunhua. Relationship Between Sedimentary Facies of Lacustrine Carbonate Rocks and Oil and Gas Distribution:A Case Study of the Tertiary Carbonate Rocks in Shengli Oilfield[J]. Petroleum Geology & Experiment, 1986, 17(2):123-132.
[34] 李红, 柳益群, 朱玉双. 新疆三塘湖盆地二叠系湖相白云岩形成机理初探[J]. 沉积学报, 2007, 25(1):75-81. Li Hong, Liu Yiqun, Zhu Yushuang. Primary Study on the Origin of Lacustrine Dolostones of Permian,Sangtanghu Basin,Xinjiang[J]. Sedimentologica Sinica, 2007, 25(1):75-81.
[35] 张代生, 李光云, 罗肇, 等. 银根-额济纳旗盆地油气地质条件[J]. 新疆石油地质, 2003, 24(2):130-133. Zhang Daisheng, Li Guangyun, Luo Zhao, et al. Characteristics of Petroleum Geology in Inggen-Ejinaqi Basin[J]. Xingjiang Petroleum Geology, 2003, 24(2):130-133.
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