岩性油气藏 ›› 2017, Vol. 29 ›› Issue (3): 5265.doi: 10.3969/j.issn.1673-8926.2017.03.007
苑伯超, 肖文华, 魏浩元, 韦德强
YUAN Bochao, XIAO Wenhua, WEI Haoyuan, WEI Deqiang
摘要: 鸭儿峡地区白垩系下沟组沟一3亚段(K1g13)是酒泉盆地的主要产油层段之一,但对其沉积相、有利储层影响因素与分布规律认识不清。以酒泉盆地鸭儿峡地区白垩系下沟组K1g13为研究对象,分析岩心、测井及室内测试等资料,探讨其沉积相类型及有利储层分布。结果表明,鸭儿峡地区下沟组K1g13主要发育扇三角洲-湖泊及近岸水下扇-湖泊两大沉积体系,可进一步识别出8种亚相、16种微相;有利储层分布受沉积相带及溶蚀带展布的双重控制。水下分流河道及河口沙坝均是主要的有利储层沉积相带,次生溶蚀孔是主要的储集空间,其发育主要受长石含量、岩屑及杂基含量、埋深等因素的控制;叠合优势沉积微相、溶蚀带分布及埋深图等,预测鸭儿峡地区白垩系下沟组K1g13有利储层分布区东以鸭西1-1-鸭西116井为界,西以鸭西115-柳10井为界,南至鸭西5井,北至鸭西112井。
中图分类号:
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