岩性油气藏 ›› 2023, Vol. 35 ›› Issue (6): 5462.doi: 10.12108/yxyqc.20230607
王雪柯, 王震, 计智锋, 尹微, 姜仁, 侯珏, 张艺琼
WANG Xueke, WANG Zhen, JI Zhifeng, YIN Wei, JIANG Ren, HOU Yu, ZHANG Yiqiong
摘要: 根据地震、钻井及薄片等资料,采用地震波阻抗储层反演技术,对滨里海盆地东缘石炭系盐下碳酸盐岩储层特征、油气成藏规律进行了研究,并指出了下一步风险勘探方向。研究结果表明:①滨里海盆地东缘石炭系盐下碳酸盐岩储层可分为灰岩类、云岩类、云灰岩/灰云岩类、硅化硅质岩类等,储层孔隙度为4%~12%,渗透率通常小于1 m D,属于低—中孔、低渗孔洞-孔隙型储层。②研究区阿克若尔构造带主要发育岩性油气藏,无统一油水界面,油层呈薄层状分散分布,对比性和连续性均较差,优质储层多为高频三级层序旋回中上部的高生长率滩体及不整合面附近的岩溶储层。③采用基于层位-测井约束的初始模型的地震波阻抗储层反演技术预测碳酸盐岩薄储层,可更清晰地呈现KT-Ⅰ和KT-Ⅱ油层组储层的纵、横向展布特征。研究区有利储层主要发育在KT-Ⅱ油层组顶部的G1和G4小层。
中图分类号:
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