首页|四川盆地茅口组一段缝洞充填物特征及成因——以A1井为例

四川盆地茅口组一段缝洞充填物特征及成因——以A1井为例

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近年来,四川盆地二叠系茅口组一段不断取得天然气发现,其泥灰岩的储集空间成因机制已成为关注的问题之一.厘米级缝洞型储集空间是茅口组一段新发现的储集空间类型之一,相关研究尚未公开报道.以四川盆地A1井为例,在岩心观察描述基础上,通过显微岩石学、碳氧同位素、锶同位素与微量元素的对比分析,研究了缝洞充填物特征及成因.茅口组一段缝洞中方解石胶结物与泥灰岩基质具有相似的碳氧同位素与锶同位素分布特征,表明方解石主要来源于围岩的溶解再沉淀;与泥灰岩相比,缝洞方解石胶结物的变价元素(V、Cr、U、Mo)、稀土元素(REE)含量降低,而微营养元素(Ni、Cu、Zn)含量升高,揭示了在此过程中微量元素的差异性迁移规律;方解石与泥灰岩基质的Mn与Sr含量的差异性变化特征揭示了成岩流体的海水亲缘属性,进一步表明其与大气淡水、深部热液流体无关.晚侏罗世以来的侧向构造推覆挤压力,形成了川东南地区滑脱断层及相关褶皱体系,在此过程中可能导致了茅口组泥灰岩变形并产生了厘米级裂缝空间.泥灰岩在后续压实—压溶作用(包括侧向压溶)等形成的成岩流体为缝洞石英和方解石胶结物提供了物质来源.
Characteristics and genesis of fillings in fracture-cavity space in first member of Permian Maokou Formation,Sichuan Basin:a case study of well A1
In recent years,natural gas discoveries have been continuously made in the first member of the Permian Maokou Formation in the Sichuan Basin,bringing attention to the genesis mechanism of marlstone reservoir space.Centimeter-scale fracture-cavity type reservoir space is one of the newly discovered types in the first member of the Maokou Formation,and relevant research has not been publicly reported.Taking well Al in the Sichuan Basin as an example,based on core observation and description,the characteristics and genesis of fracture-cavity fillings were studied through comparative analysis of microscopic petrology,carbon-oxygen isotopes,strontium isotopes,and trace elements.The similar distribution characteristics of carbon-oxygen isotopes and strontium isotopes between calcite cement and mudstone matrix in the fractures of the first member of the Maokou Formation indicated that calcite mainly came from the dissolution and redeposition of surrounding rocks.Compared with marlstone,the fracture calcite cement showed lower contents of valence elements(V,Cr,U,Mo)and rare earth elements(REE),while the content of micronutrient elements(Ni,Cu,Zn)increased,revealing the differential migration pattern of trace elements in this process.The differential variation characteristics of Mn and Sr contents between calcite and marl matrix revealed the marine affinity of diagenetic fluids,further indicating their independence from atmospheric freshwater and deep hydrothermal fluids.Since the Late Jurassic,lateral tectonic thrusting pres-sure has formed detachment faults and related fold systems in southeastern Sichuan,which potentially caused deformation of the Maokou Formation marlstone and the generation of centimeter-scale fracture spaces.Diagenetic fluids formed during subsequent compaction-dissolution processes(including lateral dissolution)provided material sources for quartz and calcite cement in the fractures.

diagenesisclay mineralmarlstoneMaokou FormationPermianSichuan Basin

孟宪武、尤东华、李蓉、宋晓波、张力钰、朱兰

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中国石化西南油气分公司勘探开发研究院,成都 610041

中国石化石油勘探开发研究院无锡石油地质研究所,江苏无锡 214126

成岩作用 黏土矿物 泥灰岩 茅口组 二叠系 四川盆地

国家自然科学基金中国石化西南油气分公司科技攻关计划

U19B6003KJ-632-2102

2024

石油实验地质
中国石油化工股份有限公司石油勘探开发研究院 中国地质学会石油地质专业委员会

石油实验地质

CSTPCD北大核心
影响因子:2.409
ISSN:1001-6112
年,卷(期):2024.46(3)
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