岩性油气藏 ›› 2023, Vol. 35 ›› Issue (6): 147158.doi: 10.12108/yxyqc.20230616
• 地质勘探 • 上一篇
唐昱哲1,2, 柴辉3, 王红军1, 张良杰1, 陈鹏羽1, 张文起1, 蒋凌志1, 潘兴明2
TANG Yuzhe1,2, CHAI Hui3, WANG Hongjun1, ZHANG Liangjie1, CHEN Pengyu1, ZHANG Wenqi1, JIANG Lingzhi1, PAN Xingming2
摘要: 以岩心、薄片及测井资料为基础,分析了中亚阿姆河右岸东部地区侏罗系牛津阶储层的岩性、储集空间及物性特征,利用三维地震数据,通过正演地震模拟、波形聚类技术、分频RGB融合技术以及集成学习等方法,对储层分布及厚度进行了半定量预测。研究结果表明:①阿姆河右岸东部地区侏罗系牛津阶储层岩性主要为生屑灰岩、颗粒灰岩及泥晶灰岩,为裂缝-孔洞型储层,储集空间以生物格架孔、粒内孔和裂缝为主,裂缝为后期溶蚀流体提供了通道;储层平均厚度为41.6 m,平均孔隙度为4.65%。②研究区储层多发育于XVhp层,根据其在XVhp层的分布位置可分为顶部型、底部型和两期型,顶部型储层主要分布于研究区中部及东部,底部型储层主要集中于西部,而两期型储层大量发育于西北部;研究区西部和东北部储层发育较好,厚度为45~75 m,多沿断裂发育带分布,东南部储层发育较差,厚度小于30 m,距离断层更远。③利用集成学习方法计算研究区储层厚度时,采用异质集成方法中的Stacking方法进行模型运算,以基于箱线图的离群值剔除方法剔除极端数据,以交叉验证法评估模型的预测性能,得到的储层厚度与11口实钻井储层厚度的变化趋势相符,相关系数为0.74。
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