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作 者:倪春华[1,2] 周小进[2] 包建平[1] 段铁军[2] 程建[2] 裴威
机构地区:[1]长江大学 地球环境与水资源学院,武汉 430100 [2]中国石化 石油勘探开发研究院无锡石油地质研究所,江苏 无锡214126 [3]无锡中关村软件园发展有限公司,江苏 无锡214135
出 处:《石油实验地质》2014年第5期583-588,共6页Petroleum Geology & Experiment
基 金:中国石化科技部项目(P10021)资助
摘 要:西非里奥穆尼盆地经历了陆内裂谷、陆间裂谷和被动大陆边缘3个构造演化阶段,发育多套烃源岩、储层及泥页岩(盐岩)盖层。以陆间裂谷阶段发育的阿普特盐岩层为界,主要形成盐上、盐下2大含油气系统。盐构造、有利储层控制了盐上含油气系统的有效成藏,优质烃源、盖层则为盐下含油气系统的关键成藏要素。综合分析认为,里奥穆尼盆地的油气勘探重点为盐上的白垩系,应寻找与盐构造相关、浊积砂体发育的构造—地层复合型油气藏;对盐下领域,应重点探索裂谷洼陷生烃中心、阿普特盐岩封盖条件好的地区,并以近源的有利构造作为优先勘探目标。Based on the background of regional structural evolution, the tectono-sedimentary evolution of Rio Muni Basin, West Africa can be divided into three phases:intracontinental rift, intercontinental rift and passive continental margin. It has been proved by exploration and research that there are multilayer source rocks, reser-voirs and caps in the basin. With the Aptian Salt developed in the intracontinental rift phase as the interface, there are pre-salt and post-salt petroleum systems. It is showed that salt structures and favorable reservoirs control the effective hydrocarbon accumulation of the post-salt system, while high-quality source rocks and caps are the key reservoir forming factors of the pre-salt system. It is recognized by comprehensive analysis that the petroleum exploration focus should be the Cretaceous on the salt and the complex hydrocarbon reservoirs with structure stra-tigraphy with the development of salt structure and turbidite sand body. It is suggested that the near-source favor-able structures are priority exploration targets to the pre-salt strata in the area located in the hydrocarbon genera-tion center of rift sag.
关 键 词:盆地演化 含油气系统 成藏条件 勘探方向 里奥穆尼盆地 西非
分 类 号:TE122.1[石油与天然气工程—油气勘探]
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