四川盆地下寒武统筇竹寺组不同岩相页岩孔隙结构差异及其主控因素OA
Pore structure differences and their controlling factors in the shales of different lithofacies in the Lower Cambrian Qiongzhusi Formation,Sichuan Basin
四川盆地下寒武统筇竹寺组页岩气资源潜力显著,是南方海相页岩气勘探的关键区域.然而,该地层岩相组成复杂且储层非均质性极强,不同岩相孔隙发育规律及其主控因素尚不明确,制约了该区域页岩气甜点优选与勘探开发部署.为此,综合利用岩心观察、薄片鉴定及地球化学分析,建立了"岩性-TOC-沉积构造-矿物"四元岩相划分方案,并结合 CO2 与 N2 吸附、高压压汞等实验手段,对不同岩相的微孔-介孔-宏孔全尺度孔隙系统进行了精细表征.分析了有机质丰度、矿物组成等多种因素对孔隙结构发育的控制作用.研究结果表明:①筇竹寺组主要发育中-高碳块状及条带状硅质页岩、贫低碳块状及纹层状硅质页岩、中-高碳块状混合质页岩及贫低碳纹层状粉砂岩 6 种岩相;②不同岩相的孔隙结构差异显著,基质孔隙体系涵盖粒间孔、粒内孔及有机质孔隙三大基本类型,裂缝系统识别出矿物颗粒边缘缝、黏土矿物层间缝及矿物收缩缝 3 类典型微裂缝;③孔隙非均质性受有机质、黏土矿物及黄铁矿协同控制,高成熟度阶段下地层压实促使介孔向微孔转化.结论认为,提出的四元岩相划分方案及孔隙差异性认识,明确了筇竹寺组页岩气储层差异性特征,可为四川盆地寒武系页岩气勘探选区及评价提供重要的理论支撑.
The Lower Cambrian Qiongzhusi Formation in the Sichuan Basin is a critical target for marine shale gas exploration in southern China due to its significant potential in shale gas resources.In this formation,however,lithofacies compositions are complex,reservoir heterogeneity is extremely strong,and the pore structures of different lithofacies and their primary controlling factors are not understood,which restrict the sweet spot selection and exploration and development arrangement of shale gas in this region.By integrating core observation,thin section identification and geochemical analysis,this paper presents a"lithology-TOC-sedimentary structure-mineral"four-element lithofacies classification scheme.Then,the micro-,meso-,and macro-pore systems of various lithofacies are finely characterized by means of CO2 and N2 adsorption,and high-pressure mercury intrusion(HPMI)experiments.Finally,the controlling roles of organic matter abundance,mineral composition and other factors on pore structure are analyzed.The following results are obtained.First,there are mainly six types of lithofacies in the Qiongzhusi Formation,including medium-high carbon massive and banded siliceous shale,low-carbon massive and laminated siliceous shale,medium-high carbon massive mixed shale,and low-carbon laminated siltstone.Second,the lithofacies are significantly different in pore structures.Matrix pore system covers three basic types,namely intergranular pore,intragranular pore and organic pore,and three types of typical microfractures are identified,including mineral particle marginal fracture,inter-clay mineral layer fracture,and mineral contraction fracture.Third,pore heterogeneity is synergistically controlled by organic matter,clay minerals and pyrite.In the high-maturity stage,formation compaction promotes the transformation of mesopores into micropores.In conclusion,the proposed four-element lithofacies classification scheme and the insights into pore variability clarify the differential characteristics of the Qiongzhusi shale gas reservoirs,providing a critical theoretical support for the selection and evaluation of Cambrian shale gas exploration areas in the Sichuan Basin.
石学文;Dmitry Koroteev;Tagir Karamov;Mohammad Nooraiepour;宋泽章;吴伟;黎丁源;赵磊;朱逸青;罗超;钟可塑;杨希希;聂美怡
中国石油西南油气田公司||页岩气地质评价与高效开发四川省重点实验室斯科尔科沃科学技术研究院斯科尔科沃科学技术研究院奥斯陆大学地球科学系油气资源与工程全国重点实验室[中国石油大学(北京)]||中国石油大学(北京)地球科学学院中国石油西南油气田公司||页岩气地质评价与高效开发四川省重点实验室中国石油西南油气田公司||页岩气地质评价与高效开发四川省重点实验室油气资源与工程全国重点实验室[中国石油大学(北京)]||中国石油大学(北京)地球科学学院中国石油西南油气田公司||页岩气地质评价与高效开发四川省重点实验室中国石油西南油气田公司||页岩气地质评价与高效开发四川省重点实验室中国石油西南油气田公司||页岩气地质评价与高效开发四川省重点实验室油气资源与工程全国重点实验室[中国石油大学(北京)]||中国石油大学(北京)地球科学学院油气资源与工程全国重点实验室[中国石油大学(北京)]||中国石油大学(北京)地球科学学院
能源科技
四川盆地孔隙结构页岩岩相海相页岩寒武系筇竹寺组
Sichuan BasinPore structureShale lithofaciesMarine shaleCambrian Qiongzhusi Formation
《天然气工业》 2026 (5)
37-53,17
国家自然科学基金面上项目"深层、超深层热液活动及其对古油藏改造效应定量表征"(编号:42272161)、中国石油天然气股份有限公司科技项目"新区新层系有利区优选与勘探评价关键技术研究"(编号:2023ZZ21YJ04)、中国石油大学(北京)学科前沿交叉探索专项"中国西部超(特)深层复合生烃机制与资源潜力"(编号:2462024XKQY001)、中国石油大学(北京)拔尖人才基金"超深层高—过成熟天然气—源对比研究"(编号:2462023BJRC023).
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