天然气地球科学

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四川盆地五峰组—龙马溪组页岩气富集特征与“建造—改造”评价思路

何治亮1,2,3,胡宗全1,2,3,聂海宽1,2,3,李双建1,2,3,许锦1,2,3   

  1. 1.页岩油气富集机理与有效开发国家重点实验室,北京 100083;
    2.中国石油化工集团公司页岩油气勘探开发重点实验室,北京 100083;
    3.中国石油化工股份有限公司石油勘探开发研究院,北京 100083
  • 收稿日期:2016-12-30 修回日期:2017-02-22 出版日期:2017-05-10 发布日期:2017-05-10
  • 作者简介:何治亮(1963-),男,湖北潜江人,教授级高级工程师,博士,主要从事石油与天然气地质学研究. E-mail:hezl.syky@sinopec.com.
  • 基金资助:

    国家重点基础研究发展计划(“973”)项目(编号:2014CB239100);国家自然科学基金项目(编号:U1663209;41202103)联合资助.

Characterization of shale gas enrichment in the Wufeng-Longmaxi Formation in the Sichuan Basin and its evaluation of geological construction-transformation evolution sequence

He Zhi-liang1,2,3,Hu Zong-quan1,2,3,Nie Hai-kuan1,2,3,Li Shuang-jian1,2,3,Xu Jin1,2,3   

  1. 1.State Key Laboratory of Shale Oil and Gas Enrichment Mechanisms and Effective Development,Beijing 100083,China;
    2.Key Laboratory of Shale Gas Exploration and Development,SINOPEC,Beijing 100083,China;
    3.Research Institute of Petroleum Exploration and Development,SINOPEC,Beijing 100083,China
  • Received:2016-12-30 Revised:2017-02-22 Online:2017-05-10 Published:2017-05-10

摘要:

四川盆地上奥陶统五峰组—下志留统龙马溪组页岩是中国目前页岩气勘探开发的重点层系之一,已发现了涪陵、威远、长宁和昭通等页岩气藏。通过页岩气藏的详细解剖,将五峰组—龙马溪组下部龙一段页岩气富集特征概括为“高、帅、富”:“高”主要指页岩层系形成页岩气的原始物质基础条件优越,有机质类型好、丰度高、脆性矿物含量高、热演化程度适中;“帅”主要表现为构造变形较晚、变形强度较弱、变形方式与构造样式有利、抬升幅度以及现今埋深适中;“富”表现为含气量高、地层压力系数大、储层物性好、有利于储层规模改造、初始产量高、最终产出量大,开发难度相对较小,经济效益明显。优越的原始沉积条件与成岩过程(地质建造作用)与后期适度的构造变形改造与抬升剥蚀(地质改造作用)的有机组合,是页岩气的富集高产前提与关键。基于“建造”(生—储演化序列)的评价内容包括层序地层与沉积、生烃和储层孔隙形成3个方面内容,基于“改造”(储—保演化序列)的评价内容主要包括构造变形、储层裂缝形成和页岩气保存2个方面。“建造—改造”的评价思路就是沿着页岩气形成与保存的全过程,既分析页岩气形成的建造条件优劣,又评价构造改造方式、程度的正面,负面影响。基于这种评价思路所建立的各种评价要素的组合模型,更符合页岩气形成与富集规律,也能更有效地消除简单将各种要素不作区别地统一纳入评价体系所带来的偏差。

关键词: 页岩气, 五峰组, 龙马溪组, 涪陵页岩气田, 富集特征, 地质建造, 地质改造, 四川盆地

Abstract:

Shale gas in the Upper Ordovician Wufeng Formation-Lower Silurian Longmaxi Formation in the Sichuan Basin is one of the key strata being explored and developed in China,where shale gas reservoirs have been found in Fuling,Weiyuan,Changning and Zhaotong.Characteristics of shale gas enrichment in the formation shown by detailed profiling and analysis are summarized as “high,handsome and rich”.“High” mainly refers to the high quality of original materials for the formation of shale with excellent key parameters,including the good type and high abundance of organic matters,high content of brittle minerals and moderate thermal evolution.“Handsome” means late and weak deformation,favorable deformation mode and structure,and appropriate uplift and current burial depth.“Rich” includes high gas content,high formation pressure coefficient,good reservoir property,favorable reservoir scale transformation and high initial and final output,with relative ease of development and obvious economic benefit.For shale gas enrichment and high yield,it is important that the combination of shale was deposited and formed in excellent conditions (geological construction),and then underwent appropriate tectonic deformation,uplift,and erosion (geological transformation).Evaluation based on geological construction (evolution sequence from formation to the reservoir) includes sequence stratigraphy and sediment,hydrocarbon generation and formation of reservoir pores.Based on geological transformation (evolution sequence from the reservoir to preservation),the strata should be evaluated for structural deformation,the formation of reservoir fracture and preservation of shale gas.The evaluation of the “construction-transformation” sequence is to cover the whole process of shale gas formation and preservation.This way,both positive and negative effects of the formation-transformation sequence on shale gas are assessed.The evaluation models based on this strategy would be more accurate,reliable and would avoid bias derived from indiscriminate and simplistic use of all parameters in the models.

Key words: Shale gas, Wufeng Formation, Longmaxi Formation, Fuling shale gasfield, Enrichment characteristics, Geological construction, Geological transformation;Sichuan Basin

中图分类号: 

  • TE122

[1]He Zhiliang,Nie Haikuan,Zhang Yuying.The main factors of shale gas enrichment of Ordovician Wufeng Formation-Silurian Longmaxi in Sichuan Basin and its adjacent areas[J].Earth Science Frontiers,2016,23(2):8-17.[何治亮,聂海宽,张钰莹.四川盆地及其周缘奥陶系五峰组—志留系龙马溪组页岩气富集主控因素分析[J].地学前缘,2016,23 (2):8-17.]
[2]Zhang Jinchuan,Nie Haikuan,Xu Bo,et al.Geological condition of shale gas accumulation in Sichuan Basin[J].Natural Gas Industry,2008,28(2):151-156.[张金川,聂海宽,徐波,等.四川盆地页岩气成藏地质条件[J].天然气工业,2008,28(2):151-156.]
[3]Nie Haikuan,Zhang Jinchuan,Bao Shujing,et al.Shale gas accumulation conditions of the Upper Ordovician-Lower Silurian in Sichuan Basin and its periphery[J].Oil & Gas Geology,2012,33(3):335-345.[聂海宽,张金川,包书景,等.四川盆地及其周缘上奥陶统—下志留统页岩气聚集条件[J].石油与天然气地质,2012,33(3):335-345.]
[4]Liu Dameng,Li Junqian,Li Zinan.Research on enrichment and accumulation mechanism of shale gas and its formation conditions in China[J].Coal Science and Technology,2013,41(9):66-70,74.[刘大锰,李俊乾,李紫楠.我国页岩气富集成藏机理及其形成条件研究[J].煤炭科学技术,2013,41(9):66-70,74.]
[5]Gao Jian,He Sheng,Yi Jizheng.Discovery of high density methane inclusions in Jiaoshiba shale gasfield and its significance[J].Oil & Gas Geology,2015,36(3):472-480.[高键,何生,易积正.焦石坝页岩气田中高密度甲烷包裹体的发现及其意义[J].石油与天然气地质,2015,36(3):472-480.]
[6]Xiao Xianming,Wang Maolin,Wei Qiang,et al.Evaluation of Lower Paleozoic shale with shale gas prospect in South China[J].Natural Gas Geoscience,2015,26(8):1433-1445.[肖贤明,王茂林,魏强,等.中国南方下古生界页岩气远景区评价[J].天然气地球科学,2015,26(8):1433-1445.]
[7]Nie Haikuan,He Faqi,Bao Shujing.Peculiar geological characteristics of shale gas in China and its exploration countermeasures[J].Natural Gas Industry,2011,31(11):111-116.[聂海宽,何发岐,包书景.中国页岩气地质特殊性及其勘探对策[J].天然气工业,2011,31(11):111-116.]
[8][KG*5/6]Nie Haikuan,Bao Shujing,Gao Bo,et al.A study of shale gas preservation conditions for the Lower Paleozoic in Sichuan Basin and its periphery[J].Earth Science Frontiers,2012,19(3):280-294.[聂海宽,包书景,高波,等.四川盆地及其周缘下古生界页岩气保存条件研究[J].地学前缘,2012,19(3):280-294.]
[9]Xiao Xianming,Wei Qiang,Gai Haifeng,et al.Main controlling factors and enrichment area evaluation of shale gas of the Lower Paleozoic marine strata in south China[J].Petroleum Science,2015,12(4):573-586.
[10]Yang R,He S,Wang X,et al.Paleo-ocean redox environments of the Upper Ordovician Wufeng and the first member in lower Silurian Longmaxi Formations in the Jiaoshiba area,Sichuan Basin[J].Canadian Journal of Earth Sciences,2016,53(4):426-440.
[11]Liang Digang,Guo Tonglou,Bian Lizeng,et al.Some progresses on studies of hydrocarbon generation and accumulation in marine sedimentary regions,Southern China (Part 3):Controlling factors on the sedimentary facies and development of Palaeozoic marine source rocks[J].Marine Origin Petroleum Geology,2009,14(2):1-19.[梁狄刚,郭彤楼,边立曾,等.中国南方海相生烃成藏研究的若干新进展(三):南方四套区域性海相烃源岩的沉积相及发育的控制因素[J].海相油气地质,2009,14(2):1-19.]
[12]Qin Jianzhong,Tao Guoliang,Tenger,et al.Hydrocarbon-forming organisms in excellent marine source rocks in South China[J].Petroleum Geology & Experiment,2010,32(3):262-269.[秦建中,陶国亮,腾格尔,等.南方海相优质页岩的成烃生物研究[J].石油实验地质,2010,32(3):262-269.]
[13]Nie Haikuan,Jin Zhijun,Bian Ruikang,et al.The “source-cap hydrocarbon controlling” enrichment of shale gas in Upper Ordovician Wufeng Formation-Lower Silurian Longmaxi Formation of Sichuan Basin and its periphery[J].Acta Petrolei Sinica,2016,37(5):557-571.[聂海宽,金之钧,边瑞康,等.四川盆地及其周缘上奥陶统五峰组—下志留统龙马溪组页岩气“源—盖控藏”富集[J].石油学报,2016,37(5):557-571.]
[14]He Zhiliang,Nie Haikuan,Zhao Jianhua,et al.Types and origin of nanoscale pores and fractures in Wufeng and Longmaxi shale in Sichuan Basin and its periphery[J].Journal of Nanoscience and Nanotechnology,2017,17(9):6626-6633.
[15]Li Shuangjian,Wo Yujin,Zhou Yan,et al.Controlling factors affect sealing capability of well-developed muddy cap rock[J].Acta Geologica Sinica,2011,85(10):1691-1697.[李双建,沃玉进,周雁,等.影响高演化泥岩盖层封闭性的主控因素分析[J].地质学报,2011,85(10):1691-1697.]

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