白豹-坪庄地区长63储层有利区块预测

根据铸体薄片、扫描电镜、岩心、测井等资料研究结果，长63储层经历了复杂的成岩作用，储层物性差，属于中低孔特低渗储层，储集空间以剩余粒间孔和溶蚀孔为主，成分成熟度低，结构成熟度中等一较高。储层质量受到沉积微相和成岩作用的双重控制．沉积微相控制着储层原生孔隙的发育，成岩作用控制着次生孔隙的发育，三角洲前缘水下分流河道水动力条件较强，沉积的碎屑物粒度相对较粗，分选好，是最有利于储层发育的沉积微相；长石溶蚀成岩相以长石溶孔发育为主要特征，长石沿解理面溶蚀强烈，次生孔隙发育，储层物性显著变好，是该区最有利的成岩相；碳酸盐胶结物溶蚀成岩相较长石溶蚀成岩相溶蚀程度低，孔隙中的铁方解石、铁白云石胶结增多，物性相对较好，是该区较有利的成岩相；绿泥石衬垫式胶结成岩相以绿泥石衬垫式充填孔隙为主要特征，胶结作用相对较弱，孔隙类型以剩余粒间孔隙为主，储层孔渗性较好，也是该区较有利的成岩相。根据沉积微相和成岩相，三角洲前缘水下分流河道和长石溶蚀成岩相、碳酸盐胶结物溶蚀成岩相以及绿泥石衬垫式胶结成岩相的叠置发育区即为该区储层有利区块。

Prediction of favorable areas of Chang 63 sandstone reservoir in Baibao-Pingzhuang Area

Based on the studies of casting thin section,scanning electron microscopy,cores,it is indicated that Chang 63 sandstone reservoir has experienced complex lithogenesis,causing the reservoir with low to medium porosity and extraordinary low permeability.The reservoir space are of mainly residual intergranular pore and corrosion pore.The compositional maturity is low and textural maturity is medium to high.The reservoir are effected by sedimentary microfacies and diagenesis,sedimentary microfacies control the ...