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川东红星地区二叠系页岩硅质成因及其地质意义

高山林 李雄 刘皓天 王惠君

古地理学报2026,Vol.28Issue(3):918-933,16.
古地理学报2026,Vol.28Issue(3):918-933,16.DOI:10.7605/gdlxb.2026.121

川东红星地区二叠系页岩硅质成因及其地质意义

Silica genesis and geological significance of the Permian shales in Hongxing area,eastern Sichuan Basin

高山林 1李雄 2刘皓天 2王惠君3

作者信息

  • 1. 中国石油化工股份有限公司油田勘探开发事业部,北京 100728
  • 2. 中国石油化工股份有限公司江汉油田分公司,湖北潜江 433124
  • 3. 中国石油化工股份有限公司江汉油田分公司勘探开发研究院,湖北武汉 430223
  • 折叠

摘要

Abstract

The genetic type of siliceous minerals exerts differential controls on shale reservoir quality;however,current reservoir evaluation frameworks predominantly employ total quartz content as a proxy,neglecting the distinct reservoir effects associated with silica of different origins.This study systematically investigates the silica origin,genesis,and geological significance of Permian shales from the Wujiaping Formation Member 2(Wu-2 Member)and Maokou Formation Member 4(Mao-4 Member)in the Hongxing area,eastern Sichuan Basin,using an integrated approach combining scanning electron microscopy with energy-dispersive spectroscopy(SEM-EDS),X-ray diffraction(XRD),and major-trace element geochemistry.The key findings are as follows:(1)Both members contain detrital quartz and biogenic quartz-the latter encompassing structurally preserved(radiolarian fossils)and structurally recrystallized(microcrystalline quartz aggregates)varieties-while hydrothermal silica is absent.The Wu-2 Member is characterized by mixed detrital-biogenic silica(absolute detrital silica content:21.7%;absolute biogenic silica content:21.22%),whereas the Mao-4 Member is dominated by biogenic silica(absolute content 20.71%)with negligible detrital input(absolute content 3.34%).(2)Two contrasting silica enrichment models are proposed:a"superimposed enrichment model"for the Wu-2 Member,where deep-water shelf conditions sustained both substantial terrigenous supply and elevated bioproductivity;and a"carbonate dilution-controlled model"for the Mao-4 Member,where pervasive carbonate minerals accumulation overwhelmingly diluted siliceous components,passively elevating the relative proportion of biogenic silica.(3)Biogenic silica content serves as positive effects for evaluating organic matter enrichment,pore preservation,and reservoir fracability.Shifting the target window in the Hongxing area from carbon-rich,medium-silica lithofacies to carbon-rich,high-silica lithofacies increased daily test gas production from 11.67×104m3 to 26.64×104m3,demonstrating the pivotal role of biogenic silica content in engineering sweet-spot selection.A comprehensive evaluation framework integrating different genetic silica content and rock mechanical parameters is therefore recommended to guide precise layer selection and efficient development of Permian shale gas in the eastern Sichuan Basin.

关键词

硅质来源/硅质成因/生物硅/储集层可压裂性/页岩/二叠系/四川盆地

Key words

silica origin/silica genesis/biogenic silica/reservoir fracability/shale/Permian/Sichuan Basin

分类

天文与地球科学

引用本文复制引用

高山林,李雄,刘皓天,王惠君..川东红星地区二叠系页岩硅质成因及其地质意义[J].古地理学报,2026,28(3):918-933,16.

基金项目

国家科技重大专项(编号:2025ZD1400403)、中国博士后科学基金项目(编号:2024M753623)和中石化科技项目(编号:P24050)共同资助.[Co-funded by the Major National Science and Technology Project of China(No.2025ZD1400403),the China Postdoctoral Science Foun-dation(No.2024M753623),and the Sinopec Science and Technology Project(No.P24050)] (编号:2025ZD1400403)

古地理学报

1671-1505

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