高邮凹陷真武油田转换式沉积演化模式  

Sedimentary evolution of Gaoyou sag in Zhenwu Oilfield

作　　者：梁琦[1] Liang Qi(Yangtze University,Wuhan 430100,China)

机构地区：[1]长江大学地球科学学院,湖北武汉430100

出　　处：《石化技术》2017年第5期134-134,共1页Petrochemical Industry Technology

摘　　要：高邮凹陷真武油田属于深凹带,经过了戴南组和三垛组两个沉积期,形成了5种主要的沉积相,这些沉积相随着物源变化、气候变化、断层活动变化以及水体运动变化等沉积环境的不同,在不同时期展现了不同的转换式沉积演化模式,对于油气藏勘探有重要的研究先导意义。Gaoyou sag in Zhenwu Oilfield is deep sag,where five main sedimentary facies are formed after Dainan and Sanduozu Formation sedimentary stage.These sedimentary facies present different sedimentary evolution at different periods with the changes of sedimentary environment such as source,climate,fault and water movement,which offers guidance for the exploration of oil and gas reservoirs.

关 键 词：高邮凹陷 真武油田 沉积相 转换式沉积演化 

分 类 号：P618.13[天文地球—矿床学]