鄂尔多斯盆地海相烃源岩系发育特征与勘探新领域

doi:10.7623/syxb201608001

石油学报 ›› 2016, Vol. 37 ›› Issue (8): 939-951,1068.DOI: 10.7623/syxb201608001

• 地质勘探 • 下一篇

鄂尔多斯盆地海相烃源岩系发育特征与勘探新领域

郭彦如¹, 赵振宇¹, 张月巧¹, 徐旺林¹, 包洪平², 张延玲¹, 高建荣¹, 宋微¹

1. 中国石油勘探开发研究院北京 100083;
2. 中国石油长庆油田勘探开发研究院陕西西安 710018

收稿日期:2016-01-02 修回日期:2016-05-26 出版日期:2016-08-25 发布日期:2016-09-02
通讯作者: 郭彦如,男,1962年6月生,1982年获西北大学学士学位,2002年获中国地质大学(北京)博士学位,现为中国石油勘探开发研究院鄂尔多斯分院副院长、高级工程师,主要从事石油天然气地质综合研究及油气勘探技术管理工作。
作者简介:郭彦如,男,1962年6月生,1982年获西北大学学士学位,2002年获中国地质大学(北京)博士学位,现为中国石油勘探开发研究院鄂尔多斯分院副院长、高级工程师,主要从事石油天然气地质综合研究及油气勘探技术管理工作。Email:guoyanru126@163.com
基金资助:
国家重大科技专项（2011ZX05004-002）及中国石油天然气集团公司重大科技专项（2014E-3201）资助。

Development characteristics and new exploration areas of marine source rocks in Ordos Basin

Guo Yanru¹, Zhao Zhenyu¹, Zhang Yueqiao¹, Xu Wanglin¹, Bao Hongping², Zhang Yanling¹, Gao Jianrong¹, Song Wei¹

1. PetroChina Research Institute of Petroleum Exploration & Development, Beijing 100083, China;
2. Research Institute of Petroleum Exploration and Development, PetroChina Changqing Oilfield Company, Shaanxi Xi'an 710018, China

Received:2016-01-02 Revised:2016-05-26 Online:2016-08-25 Published:2016-09-02

摘要/Abstract

摘要：

鄂尔多斯盆地油气勘探已进入储量发现高峰期，围绕延长组烃源岩的石油资源和来自上古生界煤系地层的天然气资源基本探明。随着盆地油气勘探的深入，急需寻找新的油气勘探接替领域。研究认为，古老海相烃源岩发育2套：即中上奥陶统海相碳酸盐岩烃源岩系和中上元古界海相碎屑岩烃源岩系。中上奥陶统海相烃源岩在不同海域有不同的特征。中奥陶统海相烃源岩发育于盆地东部华北海台内盐坳周边，以泥灰岩为主，单层厚度薄，但层系多，有机质丰度差—中等，高成熟度，有规模生烃潜力，对奥陶系盐下自源气藏有重要贡献。上奥陶统海相烃源岩主要发育于盆地西部和南部“L”型秦祁海槽斜坡相带，以泥页岩、泥灰岩为主，有机质丰度中等，累计厚度大，在天环凹陷上达到高—过成熟生气阶段，分布范围有限，在盆地西缘逆冲带上盘处于成熟生油阶段，生烃潜力较大。而中上元古界海相泥岩烃源岩系在邻区为有效烃源岩，以泥板岩为主，厚度大，有机质丰度中等，高过成熟度。在盆地本部甘陕裂陷槽新钻井中也有部分揭示。围绕2套海相烃源岩系分布的奥陶系海相碳酸盐岩和中上元古界深层海相层系是未来天然气勘探的2个新领域，其中5个有利勘探区带天然气勘探潜力大，有望形成天然气勘探接替区带。

关键词: 鄂尔多斯盆地, 海相烃源岩, 碳酸盐岩, 资源潜力, 勘探新领域

Abstract:

Oil and gas explorations in the Ordos Basin have already entered the peak period of reserves discovery. The reserves of oil resources in the source rocks of Yanchang Formation and natural gas resources in Upper Palaozoic coal measure strata have been basically ascertained. As the explorations of oil and gas in the basin progresses, it is a fairly urgent task to find new replacement exploration areas. According to the previous research results, the ancient marine source rocks are well developed in this region, including the Middle-Upper Ordovician marine carbonate source rock series and the Middle-Upper Proterozoic marine clastic source rock series. The Middle-Upper Ordovician marine source rocks exhibit different characteristics in different waters. The Middle-Upper Proterozoic marine source rocks are developed around the salt depression of Huabei Submarine Plateau in the eastern Basin, dominated by argillaceous limestones, with thin single layer and multiple series of strata. These source rocks have low-moderate abundance of organic matter and high maturity; moreover, they have large-scale hydrocarbon generation potential and make a great contribution to the Ordovician pre-salt self-source oil reserves. The Upper Ordovician marine source rocks are mainly developed in the L-shaped slope facies of the Qin-qi Trough in the western and southern Basin, dominated by shales and argillaceous limestones. These source rocks are characterized by moderate organic matter abundance and great cumulative thickness. They reached the high-postmature gas generation stage in Tianhuan Depression, with a limited distribution range. Additionally, these source rocks entered in a mature oil generation stage on the hanging side of the thrust belt along the western margin of the Basin, exhibiting great hydrocarbon generation potential. The Middle-Upper Proterozoic marine argillaceous source rocks are effective source rocks in the adjacent region, dominated by argillites and featured by moderate organic matter abundance and high postmaturity, which is also partly revealed in some new wells at the Gan-Shan Taphrogenic Trough in the Basin. The Ordovician marine carbonatites and the Middle-Upper Proterozoic deep marine strata in which the above-described two marine source rocks are extensively distributed are two new areas of natural gas exploration in the future, in which five favorable zones exhibit great exploration potentials and are expected to become the replacement zones of natural gas exploration.

Key words: Ordos Basin, marine source rock, carbonatite, resource potential, new exploration areas

中图分类号:

TE122.1

郭彦如, 赵振宇, 张月巧, 徐旺林, 包洪平, 张延玲, 高建荣, 宋微. 鄂尔多斯盆地海相烃源岩系发育特征与勘探新领域[J]. 石油学报, 2016, 37(8): 939-951,1068.

Guo Yanru, Zhao Zhenyu, Zhang Yueqiao, Xu Wanglin, Bao Hongping, Zhang Yanling, Gao Jianrong, Song Wei. Development characteristics and new exploration areas of marine source rocks in Ordos Basin[J]. Acta Petrolei Sinica, 2016, 37(8): 939-951,1068.

参考文献

[1] 刘和甫,刘立群.中国克拉通盆地演化与碳酸盐-蒸发岩层序油气系统[C]//21世纪中国油气勘探国际研讨会论文集,杭州:中国石油学会,2002,85-89.
Liu Hefu,Liu Liqun.Oil and gas system of carbonate-evaporite sequences and evolution of China craton basin[C]//The 21st century international symposium on China's oil and gas exploration,Hangzhou:China Petroleum Society,2002,85-89.
[2] Cai Liguo,Liu Hefu.Evolution and structural styles of the Sichuan foreland[C]//Xiao Xuchang,Liu Hefu.Proceeding of the 30th International Geological Congress,Holland.VSP,1997,6:87-104.
[3] 罗霞,李剑,胡国艺,等.鄂尔多斯盆地侏罗系煤生、排油能力实验及其形成煤成油可能性探讨[J].石油实验地质,2003,25(1):76-80.
Luo Xia,Li Jian,Hu Guoyi,et al.An experiment of generation and expulsion of oil from the Jurassic coals and its implication of coal generated oil in the Ordos Basin[J].Petroleum Geology&Experiment,2003,25(1):76-80.
[4] 王居峰,赵文智,郭彦如,等.鄂尔多斯盆地三叠系延长组石油资源现状与勘探潜力分析[J].现代地质,2010,24(5):957-964.
Wang Jufeng,Zhao Wenzhi,Guo Yanru,et al.Analyses of petroleum resources status and exploration potentialities,Yanchang Formation of Triassic in Ordos Basin[J].Geoscience,2010,24(5):957-964.
[5] 姚泾利,邓秀芹,赵彦德,等.鄂尔多斯盆地延长组致密油特征[J].石油勘探与开发,2013,40(2):150-158.
Yao Jingli,Deng Xiuqin,Zhao Yande,et al.Characteristics of tight oil in Triassic Yanchang Formation,Ordos Basin[J].Petroleum Exploration and Development,2013,40(2):150-158.
[6] 丁敏,姚志刚,张狄杰.鄂尔多斯盆地延长组长7页岩油存在的可能性分析[J].石油化工应用,2011,30(12):59-63.
Ding Min,Yao Zhigang,Zhang Dijie.Analysis of the existing possibility of shale oil in the Chang 7 of Erdos Basin[J].Petrochemical Industry Application,2011,30(12):59-63.
[7] 付金华,魏新善,任军峰,等.鄂尔多斯盆地天然气勘探形势与发展前景[J].石油学报,2006,27(6):1-4.
Fu Jinhua,Wei Xinshan,Ren Junfeng,et al.Natural gas exploration situation and development prospect of Ordos Basin[J].Acta Petrolei Sinica,2006,27(6):1-4.
[8] 陈孟晋,汪泽成,郭彦如,等.鄂尔多斯盆地南部晚古生代沉积特征与天然气勘探潜力[J].石油勘探与开发,2006,33(1):1-5.
Chen Mengjin,Wang Zecheng,Guo Yanru,et al.Late Paleozoic sedimentary systems and gas potential in the south Ordos Basin[J].Petroleum Exploration and Development,2006,33(1):1-5.
[9] 付金华,郭少斌,刘新社,等.鄂尔多斯盆地上古生界山西组页岩气成藏条件及勘探潜力[J].吉林大学学报:地球科学版,2013,43(2):382-389.
Fu Jinhua,Guo Shaobin,Liu Xinshe,et al.Shale gas accumulation condition and exploration potential of the Upper Paleozoic Shanxi Formation in Ordos Basin[J].Journal of Jilin University:Earth Science Edition,2013,43(2):382-389.
[10] 杨华,付金华,魏新善,等.鄂尔多斯盆地奥陶系海相碳酸盐岩天然气勘探领域[J].石油学报,2011,32(5):733-740.
Yang Hua,Fu Jinhua,Wei Xinshan,et al.Natural gas exploration domains in Ordovician marine carbonates,Ordos Basin[J].Acta Petrolei Sinica,2011,32(5):733-740.
[11] 杨华,包洪平.鄂尔多斯盆地奥陶系中组合成藏特征及勘探启示[J].天然气工业,2011,31(12):11-20.
Yang Hua,Bao Hongping.The revelation of accumulation characteristics and exploration in the Middle combination of Ordovician in Ordos Basin[J].Natural Gas Industry,2011,31(12):10-20.
[12] 郭彦如,付金华,魏新善,等.鄂尔多斯盆地奥陶系碳酸盐岩成藏特征与模式[J].石油勘探与开发,2014,41(4):393-403.
Guo Yanru,Fu Jinhua,Wei Xinshan,et al.Natural gas accumulation and models in Ordovician carbonates,Ordos Basin,China[J].Petroleum Exploration and Development,2014,41(4):393-403.
[13] 金强,黄志,李维振,等.鄂尔多斯盆地奥陶系烃源岩发育模式和天然气生成潜力[J].地质学报,2013,87(3):393-402.
Jin Qiang,Huang Zhi,Li Weizhen,et al.Sedimentary models of Ordovician source rocks in Ordos Basin and their hydrocarbon generation potential[J].Acta Geologica Sinica,2013,87(3):393-402.
[14] 张月巧,郭彦如,侯伟,等.鄂尔多斯盆地西南缘中上奥陶统烃源岩特征及勘探潜力[J].天然气地球科学,2013,24(5):894-904.
Zhang Yueqiao,Guo Yanru,Hou Wei,et al.Geochemical characteristics and exploration potential of the Middle-Upper Ordovician source rocks on the western and southern margin of Ordos Basin[J].Natural Gas Geoscience,2013,24(5):894-904.
[15] 赵振宇,郭彦如,徐旺林,等.鄂尔多斯盆地3条油藏大剖面对风险勘探的意义[J].石油勘探与开发,2011,38(1):16-22.
Zhao Zhenyu,Guo Yanru,Xu Wanglin,et al.Significance of three reservoir profiles for the risk exploration in Ordos Basin[J].Petroleum Exploration and Development,2011,38(1):16-22.
[16] 翟明国.中国主要古陆与联合大陆的形成:综述与展望[J].中国科学:地球科学,2013,43(10):1583-1606.
Zhai Mingguo.The main old lands in China and assembly of Chinese unified continent[J].Science China:Earth Sciences,2013,56(11):1829-1852.
[17] 王杰,陈践发.华北中上元古界烃源岩沉积环境及生烃潜力研究[J].天然气地球科学,2001,12(3):27-33.
Wang Jie,Chen Jianfa.The research of sedimentary environment and the hydrocarbon generation potential of hydrocarbon source rocks of Middle-Upper Proterozoic in North China[J].Natural Gas Geoscience,2001,12(3):27-33.
[18] 党振荣,张锐锋.华北油田外围新区古生界、中上元古界原生油气藏勘探[J].勘探家,1998,3(4):17-20.
Dang Zhenrong,Zhang Ruifeng.Protogenesis reservoir exploration of Palaeozoic,Middle-Upper Proterozoic in peripheral zone of Huabei Oilfield[J].Journal of Exploration,1998,3(4):17-20.
[19] 陈启林,白云来,黄勇,等.鄂尔多斯盆地寒武纪层序岩相古地理[J].石油学报,2012,33(增刊2):82-94. Chen Qilin,Bai Yunlai,Huang Yong,et al.Sequence lithofacies palaeogeography of the Cambrian in Ordos Basin,China[J].Acta Petrolei Sinica,2012,33(Supplement 2):82-94.
[20] 郭彦如,赵振宇,付金华,等.鄂尔多斯盆地奥陶纪层序岩相古地理[J].石油学报,2012,33(增刊2):95-109. Guo Yanru,Zhao Zhenyu,Fu Jinhua,et al.Sequence lithofacies palaeogeography of the Ordovician in Ordos Basin,China[J].Acta Petrolei Sinica,2012,33(Supplement 2):95-109.
[21] 张文正,杨华,李剑峰,等.鄂尔多斯盆地烃源岩研究新进展[C]//第十届全国有机地球化学学术会议论文集.无锡:中国石油学会,2005:81-84. Zhang Wenzhen,Yang Hua,Li Jianfeng,et al.Research progress of hydrocarbon source rock in Ordos Basin[C]//The 10th national conference on organic geochemistry.Wuxi:China Petroleum society,2005:81-84.
[22] 黄正良,刘燕,武春英,等.鄂尔多斯盆地奥陶系马家沟组五段中组合中下段成藏特征[J].海相油气地质,2014,19(3):57-65. Huang Zhengliang,Liu Yan,Wu Chunying,et al.Characteristics of hydrocarbon accumulation in the middle and lower sections of m iddle assemblages of Lower Ordovician Majiagou Member-5,Ordos Basin[J].Marine Origin Petroleum Geology,2014,19(3):57-65.
[23] 郝哲敏,苏中堂,王玉萍.鄂尔多斯盆地西南缘奥陶系储层类型及其空间展布[J].中国矿业,2012,21(11):75-79. Hao Zhemin,Su Zhongtang,Wang Yuping.The reservoir types and space distribution in the Ordovician on the southwest margin of Ordos Basin[J].China Mining Magazine,2012,21(11):75-79.

鄂尔多斯盆地海相烃源岩系发育特征与勘探新领域

Development characteristics and new exploration areas of marine source rocks in Ordos Basin

PDF

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	付锁堂, 金之钧, 付金华, 李士祥, 杨伟伟. 鄂尔多斯盆地延长组7段从致密油到页岩油认识的转变及勘探开发意义[J]. 石油学报, 2021, 42(5): 561-569.
[2]	张家强, 李士祥, 李宏伟, 周新平, 刘江艳, 郭睿良, 陈俊霖, 李树同. 鄂尔多斯盆地延长组7油层组湖盆远端重力流沉积与深水油气勘探——以城页水平井区长7₃小层为例[J]. 石油学报, 2021, 42(5): 570-587.
[3]	刘鹏, 王永诗, 宋明水, 刘雅利, 王敏, 张顺, 王彤达. 碳酸盐岩断裂带断层岩特征及演化——以渤海湾盆地济阳坳陷车镇凹陷下古生界为例[J]. 石油学报, 2021, 42(5): 588-597.
[4]	张友, 李强, 郑兴平, 厉玉乐, 沈安江, 朱茂, 熊冉, 朱可丹, 王显东, 齐井顺, 张君龙, 邵冠铭, 佘敏, 宋叙, 孙海航. 塔里木盆地东部古城—肖塘地区寒武纪—奥陶纪台地类型、演化过程及有利储集相带[J]. 石油学报, 2021, 42(4): 447-465.
[5]	张世铭, 王建功, 张永庶, 张小军, 张婷静, 崔俊. 柴达木盆地西部地区下干柴沟组湖相白云岩晶间孔型储层物性下限的确定[J]. 石油学报, 2021, 42(1): 45-55,118.
[6]	吴小奇, 陈迎宾, 翟常博, 王彦青, 曾华盛, 刘文汇, 杨俊, 倪春华, 周凌方, 宋晓波. 川西坳陷中三叠统雷口坡组天然气气源对比[J]. 石油学报, 2020, 41(8): 918-927,1018.
[7]	王建功, 张永庶, 李翔, 徐丽, 石亚军, 黄叶秋, 王玉林, 管斌, 张世铭, 高妍芳. 柴达木盆地西部渐新统纹理石沉积特征与原位成藏[J]. 石油学报, 2020, 41(8): 940-959.
[8]	付锁堂, 付金华, 牛小兵, 李士祥, 吴志宇, 周新平, 刘江艳. 庆城油田成藏条件及勘探开发关键技术[J]. 石油学报, 2020, 41(7): 777-795.
[9]	刘宝增, 漆立新, 李宗杰, 刘军, 黄超, 杨林, 马灵伟, 龚伟. 顺北地区超深层断溶体储层空间雕刻及量化描述技术[J]. 石油学报, 2020, 41(4): 412-420.
[10]	程洪, 汪彦, 鲁新便. 塔河地区深层碳酸盐岩断溶体圈闭类型及特征[J]. 石油学报, 2020, 41(3): 301-309.
[11]	齐宁, 陈国彬, 李振亮, 梁冲, 何龙. 基于分步算法的裂缝性碳酸盐岩油藏大尺度酸化数值模拟[J]. 石油学报, 2020, 41(3): 348-362,371.
[12]	赵靖舟, 孟选刚, 韩载华. 近源成藏——来自鄂尔多斯盆地延长组湖盆东部“边缘”延长组6段原油的地球化学证据[J]. 石油学报, 2020, 41(12): 1513-1526.
[13]	王宜林, 宋新民, 王贵海, 汪华, 李兆明, 张红, 聂臻. 中东地区油气合作区快速规模上产关键技术与实践[J]. 石油学报, 2020, 41(12): 1633-1642.
[14]	李向东, 陈海燕. 深水环境下古水流方向分析和阻塞浊流沉积的识别——以鄂尔多斯盆地桌子山地区上奥陶统拉什仲组为例[J]. 石油学报, 2020, 41(11): 1348-1365.
[15]	郭建春, 任冀川, 王世彬, 苟波, 赵俊生, 伍林. 裂缝性致密碳酸盐岩储层酸压多场耦合数值模拟与应用[J]. 石油学报, 2020, 41(10): 1219-1228.