微层序（microsequence）是在野外露头上能够以常规方法识别的最小沉积层序单元。限于浅水环境发育，与一般所用副层序（parasequence）的时限大致相当，约为0.02～0.04百万年，可能与米兰柯维奇长周期相比。
证实此种方法在划分微层序上是一种新的工作方法。
It proves that this method is a new one in the dividing micro-sequnce.
在对地表露头的微相分析基础上，对吉木萨尔地区仓房沟群进行高分辨率层序地层学研究。
High resolution sequence stratigraphy of Cangfanggon Group in Jimusa'er Area is studied based on a microfacies analysis of surface outcrop.
在高频层序内研究了沉积微相的构成与演化特征以及储层分布规律。
The constitution and evolution features of sedimentary facies and reservoir distribution rules are studied within the high frequency sequence.
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