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1)  siltstone reservoir
粉砂岩储层
1.
Study on sensitivity of siltstone reservoir of Saling formation in Daqing oilfield;
大庆油田萨零组粉砂岩储层敏感性研究
2)  siltstone reservoir
粉砂岩储集层
3)  sand reservoir
砂岩储层
1.
Fracture characteristics and fuzzy recognition techniques of Chenbao sand reservoir in Subei basin;
苏北盆地陈堡砂岩储层裂缝特征及模糊识别技术
4)  sandstone reservoirs
砂岩储层
1.
Study of permeability of sandstone reservoirs based on fractal theory;
基于分形理论预测砂岩储层渗透率
2.
Coarse clastic fan-delta, lacustrine fan sandstone reservoirs are deve.
经过初陷—裂陷、扩张和再陷三个构造—沉积演化期 ,区内沉积了以源近流短的扇三角洲、湖底扇等为主的粗碎屑砂岩储层。
3.
By comprehensive analyses and investigations, the low-permeability sandstone reservoirs in Jurassic are classified into six types based on their origin.
羌塘盆地侏罗系地层厚度大 ,分布面积广 ,砂岩储层发育 ,但砂岩储集物性及孔隙结构普遍较差 ,现有露头样品分析表明 ,其储层主要为低特低渗储层。
5)  reservoir sandstone
储层砂岩
1.
Authigenic mineral assemblage and two types of diagenetic ambient found in the Meso-Cainozoic reservoir sandstones in Tarim basin.;
塔里木盆地中新生界储层砂岩自生矿物组合与两种成岩环境
2.
Authigenic kaolinite distribution and origin in Paleogene and Neogene reservoir sandstones in Xihu sag;
西湖凹陷古近系及新近系储层砂岩自生高岭石分布特征及形成机制
3.
This paper primarily discusses the changeable features of the process through the modelling experiment of secondary migration using the reservoir sandstone with ultra-low porosity and permeability.
石油二次运移是一个复杂的地质过程 ,本文通过利用饱和地层水的低孔低渗储层砂岩来进行石油二次运移模拟实验 ,初步研究了此过程的变化特征。
6)  sandstone reservoir
砂岩储层
1.
Experimental evaluation on formation damage caused by re-injection of mixture of fresh water and produced water in sandstone reservoir;
砂岩储层清水和污水混注对储层损害的实验评价
2.
Significance of synsedimentary volcanism for formation of sandstone reservoirs of the Upper Paleozoic in Ordos Basin;
同沉积期火山作用对鄂尔多斯盆地上古生界砂岩储层形成的意义
3.
Evolution of sandstone reservoirs in the Lower Jurassic Xiaomeigou Formation,Shiquantan area,Qaidam basin;
柴达木盆地石泉滩地区下侏罗统小煤沟组砂岩储层演化特征
补充资料:粉砂岩
粉砂岩
siltstone

   由粒径为0.0625~0.0039毫米(mm)的粉砂的含量占50%以粉砂岩标本的一种碎屑沉积岩。除粉砂以外其它由砂、粘土或化学沉淀物组成。按粒度划分为粗粉砂岩(0.0625~0.0312mm)和细粉砂岩(0.0312~0.0039mm)。按碎屑成分划分为石英粉砂岩、长石粉砂岩、岩屑粉砂岩(少见)和它们间的过渡类型。根据胶结物成分划分为粘土质粉砂岩、铁质粉砂岩、钙质粉砂岩和白云质粉砂岩。黄土也是一种疏松的或半固结的粉砂质沉积物。粉砂岩多形成于河漫滩、三角洲、潟湖和海洋的较深水部位。
    
   

粉砂岩标本

粉砂岩标本

说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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