作者:刘丽;赵应成;王友净;李佳鸿;闫林辉;惠钢;刘畅; 时间:2015-01-01 点击数:
刘丽;赵应成;王友净;李佳鸿;闫林辉;惠钢;刘畅;
1:中国石油天然气股份有限公司勘探开发研究院
摘要(Abstract):
利用岩心、薄片、扫描电镜、X线衍射等资料,研究华庆B153井区长63重力流储层特征、发育控制因素及成因机制.结果表明:长63储层为典型的超低渗储层,岩石类型以长石砂岩和岩屑长石砂岩为主,储集空间以残余原生粒间孔隙为主,溶蚀孔隙次之;储层物性差,非均质性强,受沉积相、岩石矿物组成和成岩演化的综合控制,强压实作用、绿泥石胶结作用、碳酸盐胶结作用及弱溶蚀作用是导致储层低孔、低渗的关键成岩作用;根据不同成岩作用对储层物性影响的强弱程度,将超低渗储层成因机制划分为碳酸盐胶结低渗型、绿泥石胶结—溶蚀低渗型及强压实改造低渗型3种.应用孔隙度反演回剥方法,重建各成因机制低渗储层的致密化过程,为研究区有利储层预测提供地质依据.
关键词(KeyWords):超低渗储层;重力流;成因机制;致密化过程;华庆B153井区
Abstract:
Keywords:
基金项目(Foundation):中国石油重大科技专项(2011B-1205)
作者(Author):刘丽;赵应成;王友净;李佳鸿;闫林辉;惠钢;刘畅;
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