指出飞仙关组滩体发育于研究区东北部，呈点状不连续分布。
It is pointed out that the oolitic beach are developed discontinuous in the north east.
沉积后期成岩作用的不均一性是造成各类储集层平面不连续分布特征的主要因素。
Moreover, the heterogeneity characteristics of post sedimentary diagenesis caused the isolated and discontinuous planar distribution of all types of reservoir.
贝壳中的方解石和文石层均呈多级超微结构，微量的有机质在晶界和晶内呈不连续分布。
The calcite layer and aragonite layers are multi-scale structure , and a small quantity of organic matrix distributes mainly in their grain boundary.
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