川中地区上三叠统须家河组储层成岩相

利用铸体薄片、阴极发光、扫描电镜等资料，对川中地区上三叠统须家河组储层成岩作用类型及特征进行了综合研究，在此基础上划分成岩相类型，建立了不同类型成岩相测井曲线特征，进行了研究区须家河组成岩相纵向及平面分布研究。结果表明，研究区须家河组碎屑岩储层经历了机械压实、硅质胶结、碳酸盐胶结破坏性成岩作用及溶蚀、绿泥石胶结建设性成岩作用。将储层划分为低孔特低渗溶蚀相、特低孔超低渗压实 溶蚀相、致密强压实相、致密硅质胶结相、致密方解石胶结相5种成岩相类型。低孔特低渗溶蚀相及特低孔超低渗压实 溶蚀相主要分布在须二段、须四段与须六段下部，致密强压实相、致密硅质胶结相、致密方解石胶结相在纵向及横向上封隔有利成岩相，形成岩性圈闭。平面上将川中地区须家河组储集层划分为低孔特低渗溶蚀相、特低孔超低渗压实 溶蚀相及致密强压实相分布区。

Reservoir diagenetic facies of the Upper Triassic Xujiahe Formation in the central Sichuan Basin

Based on data of cast-slice,cathodeluminescence and SEM analyses data,the present paper comprehensively investigated types and characteristics of reservoir diagenesis of the Upper Triassic Xujiahe Formation in the central Sichuan Basin,distinguished types of diagenetic facies,discussed logging curve features of diagenetic facies,and examined vertical and lateral distributions of diagenetic facies.The results demonstrated that clastic reservoirs of the Xujiahe Formation in the studied area experienced destru...