1) sandstone core
砂岩岩心
1.
The pore structure,oil and water flow mechanics including the lithology of sandstone core,electricity curve and relative permeability curve were characterized by fractal.
砂岩岩心不仅孔隙结构具有分形特征,而且油、水在岩石内部渗流过程中岩电特性曲线和油、水相对渗透率曲线也具有分形特征。
2) True sandstone micro-model
岩心砂岩模型
5) sandstone lithology
砂岩岩性
1.
Based on preliminary experiment data, this paper discusses the possible impact of sandstone lithology, percentage of smectite layers in interstratified illite/smectite, and development of chlorite on authigenic illites K-Ar system in oil/gas reservoirs, and concludes that for being used in this technique, medium-fine sandsto.
对油气储层中自生伊利石K Ar体系产生影响的有关问题如砂岩岩性、伊利石 /蒙皂石间层矿物的间层比和绿泥石进行了初步试验和讨论。
6) sandstone pressure bump
砂岩岩爆
1.
2 tunnel s left line,this paper makes corresponding analysis on the mechanism and causes of the geological disasters such as the sandstone pressure bump,and landslide,etc.
结合铁峰山2#隧道左线出口段的施工情况,针对性地分析了砂岩岩爆和塌方等地质灾害产生的机理和原因,提出了不同的应变防治措施,取得了良好的效果,可对以后类似隧道的设计和施工起到一定的借鉴作用。
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。
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