Diagenesis and implication for the reservoir quality of the tight sandstone reservoir in the depression zone of foreland basin, Upper Triassic Xujiahe Formation, Western Sichuan Foreland Basin, China: Evidence from petrography and geochemistry
{"title":"Diagenesis and implication for the reservoir quality of the tight sandstone reservoir in the depression zone of foreland basin, Upper Triassic Xujiahe Formation, Western Sichuan Foreland Basin, China: Evidence from petrography and geochemistry","authors":"Peng Huang , Ming-Jie Liu , Bo Cao , Zi-Long Wang","doi":"10.1016/j.petsci.2025.12.016","DOIUrl":null,"url":null,"abstract":"<div><div>Tight sandstones are products of complex and various diagenetic events that significantly affect reservoir quality and heterogeneity. In this study, tight sandstones of the Upper Triassic Xu3 Member in the Western Sichuan Foreland Basin were examined as a case study. Petrographic and geochemical analyses were combined to investigate diagenetic variability and its effects on reservoir quality. The sandstone in this zone consisted of coarse-grained to siltstone-grained poorly to moderately sorted sublitharenite and litharenite. And the sandstone exhibits poor physical properties. The diagenesis during the eodiagenetic stage included compaction, dissolution, early-stage quartz cementation, early-stage carbonate cementation (calcite and dolomite), and kaolinite formation. The mesodiagenetic stage encompassed compaction, dissolution, late-stage quartz cementation, intermediate- and late-stage carbonate cementation (ferro-calcite, ankerite, and calcite in fractures), and clay cementation (kaolinite, illite, and chlorite). Compaction destroyed the tight sandstone reservoir to a greater degree than cementation. Specifically, compaction and cementation reduced the initial porosity by 80.70% and 15.50%, respectively. Dissolution emerges as primary constructive diagenesis, promoting the formation of authigenic minerals. The vertical variability in dissolution and cementation within the cycle contributed to increased reservoir heterogeneity. Relatively high-quality reservoirs in the sandstone overlaying sandstone style occurred at the base of the cycle. In the mudstone overlaying sandstone style, relatively high-quality reservoirs developed at both the base and the top of the sandstone layers. These findings enhance our understanding of diagenetic influences on reservoir properties and the distribution of high-quality reservoirs. Consequently, they offer valuable insights for advancing unconventional oil and gas exploration in depression zones of foreland basins.</div></div>","PeriodicalId":19938,"journal":{"name":"Petroleum Science","volume":"23 4","pages":"Pages 1650-1674"},"PeriodicalIF":6.1000,"publicationDate":"2026-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Petroleum Science","FirstCategoryId":"5","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1995822625004960","RegionNum":1,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"2025/12/13 0:00:00","PubModel":"Epub","JCR":"Q2","JCRName":"ENERGY & FUELS","Score":null,"Total":0}
引用次数: 0
Abstract
Tight sandstones are products of complex and various diagenetic events that significantly affect reservoir quality and heterogeneity. In this study, tight sandstones of the Upper Triassic Xu3 Member in the Western Sichuan Foreland Basin were examined as a case study. Petrographic and geochemical analyses were combined to investigate diagenetic variability and its effects on reservoir quality. The sandstone in this zone consisted of coarse-grained to siltstone-grained poorly to moderately sorted sublitharenite and litharenite. And the sandstone exhibits poor physical properties. The diagenesis during the eodiagenetic stage included compaction, dissolution, early-stage quartz cementation, early-stage carbonate cementation (calcite and dolomite), and kaolinite formation. The mesodiagenetic stage encompassed compaction, dissolution, late-stage quartz cementation, intermediate- and late-stage carbonate cementation (ferro-calcite, ankerite, and calcite in fractures), and clay cementation (kaolinite, illite, and chlorite). Compaction destroyed the tight sandstone reservoir to a greater degree than cementation. Specifically, compaction and cementation reduced the initial porosity by 80.70% and 15.50%, respectively. Dissolution emerges as primary constructive diagenesis, promoting the formation of authigenic minerals. The vertical variability in dissolution and cementation within the cycle contributed to increased reservoir heterogeneity. Relatively high-quality reservoirs in the sandstone overlaying sandstone style occurred at the base of the cycle. In the mudstone overlaying sandstone style, relatively high-quality reservoirs developed at both the base and the top of the sandstone layers. These findings enhance our understanding of diagenetic influences on reservoir properties and the distribution of high-quality reservoirs. Consequently, they offer valuable insights for advancing unconventional oil and gas exploration in depression zones of foreland basins.
期刊介绍:
Petroleum Science is the only English journal in China on petroleum science and technology that is intended for professionals engaged in petroleum science research and technical applications all over the world, as well as the managerial personnel of oil companies. It covers petroleum geology, petroleum geophysics, petroleum engineering, petrochemistry & chemical engineering, petroleum mechanics, and economic management. It aims to introduce the latest results in oil industry research in China, promote cooperation in petroleum science research between China and the rest of the world, and build a bridge for scientific communication between China and the world.