摘要
本文系统论述了位于塔中隆起北部斜坡带上的塔中32井钻遇地层的沉积相类型及相模式，并对主要目的层段进行了层序地层分析。首次提出中上奥陶统为受潮汐作用和风暴作用两种能量控制的混积陆棚相沉积的观点。并认为下志留统属滨岸相沉积，而石炭系则为一套海陆过渡相的沉积。
This paper analyzed the type of sedimentary facies and facies models of Tazhong No. 32 well in the Northern slope of Tazhong uplift. It is considered firstly that Mid - upper ordovician is neritic shelf facies controlled by tide process energy and storm process energy.
出处
《新疆石油学院学报》
1998年第2期1-9,共9页
Journal of Xinjiang Petroleum Institute
关键词
沉积相
层序地层
盆地
油气勘探
Tarim Basin, sedimentary facies, sequence stratigraphy, Tazhong No.32 well
