岩性油气藏 ›› 2019, Vol. 31 ›› Issue (5): 7083.doi: 10.12108/yxyqc.20190508
李百强1, 张小莉1, 王起琮2, 郭彬程3, 郭艳琴2, 尚晓庆2, 程浩2, 卢俊辉1, 赵希1
LI Baiqiang1, ZHANG Xiaoli1, WANG Qicong2, GUO Bincheng3, GUO Yanqin2, SHANG Xiaoqing2, CHENG Hao2, LU Junhui1, ZHAO Xi1
摘要: 为研究低渗—特低渗白云岩储层的成岩相测井识别方法并进行定量划分,明确白云岩成岩相的空间展布及其有利区,依据岩心观察、普通薄片和铸体薄片鉴定、以及阴极发光分析等,结合X射线衍射和物性资料,对伊陕斜坡中东部马五段白云岩储层的成岩环境及成岩作用进行剖析,通过测井曲线的交会分析与软件的综合应用,构建了低渗—特低渗白云岩储层成岩相的定量识别标准。结果表明,低渗—特低渗白云岩储层成岩相可划分为早期大气淡水溶蚀亚相、表生期大气淡水溶蚀亚相、浅埋藏活跃回流渗透云化亚相、浅埋藏隐伏回流渗透云化亚相、钙质胶结相和泥质充填相等6类;以Pe-DEN,RLLD-DEN交会及RLLD-AC交会为代表的测井参数交会图法及软件综合应用是进行低渗—特低渗白云岩储层不同成岩相单井纵向上定量识别与连续划分的有效方法;白云岩储层成岩相在空间的分布具有纵向分带、横向分区的典型特征。有利储层主要分布于早期大气淡水溶蚀亚相和浅埋藏活跃回流渗透云化亚相,其次为表生期大气淡水溶蚀亚相,浅埋藏隐伏回流渗透云化亚相储层分布最少。
中图分类号:
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