组成江汉盆地潜江凹陷潜江组盐间段非砂岩储层的岩石主要为泥晶白云岩、钙芒硝岩、泥岩及其混积岩，孔渗性普遍较差。
Nonsandstone reservoirs between salt beds of Qianjiang Formation in the Qianjiang Sag of the Jianghan Basin are mainly composed of dolomicrite, glauberite rock, mudstone and their peperite.
研究区砂岩储层的孔隙分布较为集中，储集层非均质性主要由喉道非均质性引起。
The pore distribution of the sandstone reservoir is comparatively centralized. The reservoir inhomogeneity is mainly caused by the throat inhomogeneity.
综合分析认为，引起储层非均质性的主要原因是沉积环境的变化。
By analyses, the main reason of poor reservoir heterogeneity is the change of depositional environment.
四川盆地下二叠统中次生白云岩及古岩溶是下二叠统主要的非构造圈闭储层之一。
The secondary dolomite and paleokarst of the Lower Permian Series in Sichuan basin is one of the important atectonic reserviors in the basin.
引起储层非均质性的主要原因是沉积环境和构造环境。
Primary reasons leading to reservoir heterogeneity are sedimentary environment and tectonism.
研究区葡萄花油层段储层主要为中孔低渗储层，砂体连通性差，非均质性强。
Putaohua oil bearing reservoir primarily is middle prosperous and low permeable with sand bodies of bad conjunction and high heterogeneity.
复杂储集空间储集层的测井解释一直是测井解释工作的难题之一，其主要原因是由于储层的强烈非均质性造成的。
The logging interpretation of complex pore structure reservoirs has always been a tough job due to the severe inhomogeneous property of reservoirs.
油藏边水及储层非均质性是影响剩余油分布的主要因素。
The edge water and the heterogeneity of the reservoir are the main factors of influencing the remaining oil distribution.
本文主要介绍了被注入到储层中的非牛顿流体水动力参数的测定表达式及推导过程。
This paper introduces the hydrodynamic parameter expression of non-Newtonian fluid being injected into the reservoir.
这种储层主要是泥岩，含盐和白云石，裂缝发育，并且岩性变化大。决定盐间非砂岩储层敏感性相当复杂。
These reservoirs are mainly contained mudstone, with salts and dolomite, fracture growth, and variational reservoir lithology, which determine reservoir sensitivities are very complicated.
砾岩油藏驱油效率主要受储层微观孔隙结构特征、储层宏观非均质性特征、原油粘度和注水政策的影响。
The Results shows that the oil displacement efficiency is mainly affected by pore structure, macro heterogeneity, oil viscosity and technology policy of water flooding.
砂岩储层的微观非均质性主要由砂岩孔隙特征、粘土矿物和孔喉分布等表征。
The microheterogeneity in the sand reservoirs is represented by the pore nature, clay mineral composition and pore throat distribution.
分析了近源沉积物、成岩作用及粘土矿物演化对低渗透储层物性的影响，复杂的成岩作用是低渗透储层非均质性的主要成因。
These influence of physical property of low permeable reservoir by the sediment of short source, diagenesis and evolution of clay minerals are analysed.
分析了近源沉积物、成岩作用及粘土矿物演化对低渗透储层物性的影响，复杂的成岩作用是低渗透储层非均质性的主要成因。
These influence of physical property of low permeable reservoir by the sediment of short source, diagenesis and evolution of clay minerals are analysed.
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