岩性油气藏 ›› 2021, Vol. 33 ›› Issue (1): 186197.doi: 10.12108/yxyqc.20210117
张闻亭1, 龙礼文1, 肖文华2, 魏浩元2, 李铁锋2, 董震宇2
ZHANG Wenting1, LONG Liwen1, XIAO Wenhua2, WEI Haoyuan2, LI Tiefeng2, DONG Zhenyu2
摘要: 下白垩统下沟组沟零段(K1g0)、沟一段(K1g1)为酒泉盆地青西凹陷窟窿山构造带的主力产层,为明确其沉积特征及有利储层分布,利用岩心、测井、地震及分析化验等资料,开展了高分辨率层序地层划分、物源分析、沉积微相展布研究,阐述了储层特征及主控因素,基于储层综合评价划分了储层类型,并运用深度学习非线性反演技术预测了有利储层分布。结果表明:酒泉盆地青西凹陷窟窿山构造带下沟组K1g0—K1g1自下而上可划分为4个中期基准面旋回(MSC1—MSC4)和8个短期基准面旋回(SSC1—SSC8);窟窿山构造带下沟组K1g0—K1g1以退积型扇三角洲为主,发育西部、南部、东部3个物源,扇三角洲在K1g0和K1g1中下部均发育程度高,展布范围广;裂缝是改善储层物性的重要因素,与次生孔隙共同构成主要的储集空间,可划分为孔隙型储层、孔隙-裂缝型储层和致密型储层。利用深度学习非线性反演技术预测有利储层面积14.7 km2。该研究成果可为窟窿山构造带下白垩统油气勘探提供借鉴。
中图分类号:
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