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四川盆地上三叠统须家河组致密砂岩成储机制

金值民 冯斌豪 郑超 张修涛 刘章昊 马勇 张奥博 霍利娜 姜福杰 秦长彩 曹流

石油实验地质2026,Vol.48Issue(4):860-874,15.
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石油实验地质2026,Vol.48Issue(4):860-874,15.DOI:10.11781/sysydz2026040860

四川盆地上三叠统须家河组致密砂岩成储机制

Reservoir formation mechanism of tight sandstones of the Upper Triassic Xujiahe Formation in the Sichuan Basin:new insights based on source control

金值民 1冯斌豪 2郑超 1张修涛 2刘章昊 1马勇 2张奥博 1霍利娜 2姜福杰 2秦长彩 2曹流2

作者信息

  • 1. 中国石油西南油气田分公司勘探开发研究院,四川成都 610041
  • 2. 油气资源与工程全国重点实验室中国石油大学(北京),北京 102249||中国石油大学(北京)地球科学学院,北京 102249
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摘要

Abstract

The Upper Triassic Xujiahe Formation in the Sichuan Basin hosts one of China's most important tight sandstone gas reservoirs.To clarify the reservoir development mechanism under a multi-provenance framework,reservoir characteristics and the principal controlling factors associated with four major provenance systems-the Jiangnan Old Land,the Micangshan-Dabashan Fold Belt,the Kangdian Old Land,and the Longmenshan Thrust Belt-were systematically compared across the entire basin using core observations,thin-section petrography,X-ray diffraction(XRD),and high-pressure mercury intrusion(HPMI)analyses.Based on these results,the development pattern of high-quality reservoirs was established.Reservoirs sourced from different provenance systems exhibit significant differences in lithic composition and compositional maturity.The 2nd member of the Xujiahe Formation(Xu 2 Member)is dominated by lithic sandstone,whereas carbonate lithic fragments become more abundant in the 3rd member(Xu 3 Member).The 4th member(Xu 4 Member)exhibits the most favorable reser-voir properties.The reservoirs are generally characterized by ultra-low porosity(average 6.0%-10.8%)and ultra-low to extremely low permeability(average(0.005-2.238)× 10-3 μm2).Reservoir space is dominated by secondary dissolution pores,with primary pores occurring as a subordinate component.Specifically,the Xu 4 Member exhibits the optimal pore-throat structure,whereas the southeastern Sichuan provenance area displays the highest mercury withdrawal efficiency(average 38.57%)and the best pore-throat connectivity.Compaction is the primary destructive diagenetic process,followed by cementation(characterized by siliceous and calcareous cements);conversely,dissolution(specifically of feldspar and lithics)effectively improves the pore space.Com-paction is strongest in the northwestern Sichuan provenance area,while dissolution is most developed in the southeastern Sichuan provenance area.The development of high-quality reservoirs is synergistically controlled by four factors:provenance systems providing the geological foundation,sedimentary microfacies determining reser-voir quality,differential diagenesis controlling pore evolution,and fractures enhancing reservoir connectivity.Distributary channel sand bodies within braided river deltas exhibit the best physical properties,and fractures development significantly enhances the reservoir permeability in the study area.This study provides a theoretical foundation for sweet-spot optimization and the efficient exploration and development of tight sandstone gas reser-voirs within the Xujiahe Formation in the Sichuan Basin.

关键词

多物源体系/成岩作用/主控因素/致密砂岩储层/须家河组/四川盆地

Key words

multi-provenance system/diagenesis/main controlling factor/tight sandstone reservoir/Xujiahe Formation/Sichuan Basin

分类

能源科技

引用本文复制引用

金值民,冯斌豪,郑超,张修涛,刘章昊,马勇,张奥博,霍利娜,姜福杰,秦长彩,曹流..四川盆地上三叠统须家河组致密砂岩成储机制[J].石油实验地质,2026,48(4):860-874,15.

基金项目

国家自然科学基金项目(42173030)和国家科技重大专项(2025ZD1400400)联合资助. (42173030)

石油实验地质

1001-6112

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