天然气地球科学

• 天然气地质学 • 上一篇    下一篇

四川盆地元坝_通南巴地区须家河组致密砂岩储层成岩—成藏耦合关系

李军1,胡东风2,邹华耀3,李平平3   

  1. 1.西安石油大学地球科学与工程学院,陕西 西安 710065;
    2.中国石化勘探南方分公司,四川 成都 610041;
    3.中国石油大学(北京) 油气资源与探测国家重点实验室,北京 102249
  • 收稿日期:2015-12-14 修回日期:2016-02-17 出版日期:2016-07-10 发布日期:2016-07-10
  • 作者简介:李军(1982-),男,重庆万州人,讲师,博士,主要从事油气成藏地质学、非常规油气地质与勘探研究. E-mail:lijun@xsyu.edu.cn.
  • 基金资助:
    国家自然科学基金(编号:41472118;41502132);西安石油大学青年科技创新基金(编号:2013BS018)联合资助.

Coupling relationship between reservoir diagenesis and gas accumulationin Xujiahe Formation of Yuanba-Tongnanba area,Sichuan Basin,China

Li Jun1,Hu Dong-feng2,Zou Hua-yao3,Li Ping-ping3   

  1. 1.School of Earth Sciences and Engineering,Xi’an Shiyou University,Xi’an 710065,China;
    2.South Company of Prospecting,SINOPEC,Chengdu 610041,China;
    3.State Key Laboratory of Petroleum Resource and Prospecting,China University of Petroleum,Beijing 102249,China
  • Received:2015-12-14 Revised:2016-02-17 Online:2016-07-10 Published:2016-07-10

摘要: 储层致密期与天然气充注期的关系是致密砂岩气成藏机理及富集规律研究中尚未得到很好解决的关键问题。主要基于对四川盆地元坝_通南巴地区须家河组致密砂岩成岩演化史、天然气充注历史和致密砂岩储层有机_无机水岩相互作用序列的分析,总结了四川盆地元坝_通南巴地区须家河组致密砂岩储层致密化机理,厘定了储层致密期与天然气成藏期的关系。指出早期强的压实作用使储层物性大幅降低及其导致的半封闭_封闭成岩流体系统是致密储层形成的主要原因。后期半封闭_封闭成岩流体系统中,流体流通不畅,溶蚀作用产物迁移受阻,以就地沉淀形成胶结物为主,堵塞溶蚀孔隙和剩余原生孔隙,溶蚀作用越强胶结物含量也越高,从而使储层进一步致密化。须家河组烃源岩生排烃史和储层流体包裹体特征研究表明,天然气的充注发生在中侏罗世_早白垩世,以早白垩世为主。综合储层致密史、天然气充注史和有机_无机水岩相互作用序列分析认为天然气充注时储层已经致密,具有储层先致密天然气后成藏的特征。

关键词: 须家河组, 成岩作用, 致密化过程, 充注历史, 成岩_成藏耦合关系, 元坝_通南巴地区

Abstract: The relationship between reservoir tighting time and gas charge period is the key issue which has not been well solved in studies on the tight sand gas accumulation mechanism and enrichment regularity.Based on the analysis of diagenetic evolution history,interaction sequence of organic-inorganic in aquiferous rock and gas charge history,the tighting mechanism of tight sandstone reservoir and the relationship between reservoir tighting time and gas accumulation period of Xujiahe Formation have been analyzed in Yuanba-Tongnanba area of Sichuan Basin.It has been confirmed that the main reason for the tight sandstone reservoir formation is the intensive mechanical compaction which dramatically reduce sandstone reservoir quality and resulted in semi-closed to closed diagenetic fluid system formation at early diagenetic stage.In the semi-closed to closed diagenetic fluid system,at the later diagenetic stage,the fluid circulation is not smooth,and the migration of dissolution products is blocked,so the dissolution products mainly undergo the in situ precipitation and cementation.Such dissolution products block the dissolution pores and residual primary pores,and the stronger the dissolution,the higher the cement content is,which makes the reservoir further tightened.The hydrocarbon generation,expulsion history of source rocks and reservoir fluid inclusion characteristics in Xujiahe Formation show that the charge of natural gas occurs in the Middle Jurassic-Early Cretaceous(mainly Early Cretaceous).Comprehensive analysis of reservoir tighting history,gas charge history and interaction sequence of organic-inorganic aquiferous in rock indicated that the sandstone reservoir was experiencing tighting process when gas charged in Xujiahe Formation in Yuanba-Tongnanba area of Sichuan Basin.

Key words: Xujiahe Formation, Diagenesis, Tighting process, Charge history, Coupling relationship between diagenesis and accumulation, Yuanba-Tongnanba area of Sichuan Basin

中图分类号: 

  • TE122.2

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