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siltstone相关的网络例句

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与 siltstone 相关的网络例句 [注:此内容来源于网络,仅供参考]

The paper introduced serious sand production actuality of the quaternary gas reservoir located in Sebei Gas Field,which consists of unconsolidated fine siltstone formations with high content of shale.

介绍了涩北气田第四系高泥质疏松粉细砂岩气藏的出砂现状,通过多年的室内基础理论研究和现场防砂先导性试验成果总结,形成了适合涩北气田的高压一次充填防砂工艺。

The gas hydrates are preserved in the pores and cracks of the siltstone layers sandwiched in the oil shale member of the Middle Jurassic Jiangcang Formation. The gas in the gas hydrates is dominated by heavy hydrocarbons, with the methane accounting up to 52%~68%.

通过对钻获天然气水合物样品的分析,以及对以往异常可燃气体涌出钻孔的测井曲线的重新解释和对比分析,初步确定天然气水合物赋存于中侏罗统江仓组油页岩段的细粉砂岩夹层内的孔隙和裂隙中。

On the basis of the laboratory data and by widely analysing the formation origin and mechanism of low-resistivity oil/gas reservoir, a point of view is put forward which is not consistent with the idea existing for a long time, that is not all the low-resistivity oil/gas reservoir is shaly sandstone. Fine grains or pure fine siltstone can also form the low-resistivity oil/gas reservoir. And the additional conductibility of clay will become the prominent factor that causes the low-resistivity only when the salinity of formation water is lower. Actual cases indicate that when the salinity of formation water is greater than 300000ppm or so, even ifthere is some clay, its additional conductibility can also be ignored.

建立在实验室数据的基础之上,并通过广泛地低电阻率油气储集层成因和机理分析,提出了与长期以来存在于人们头脑中的思想观念不相一致的看法,即认为低电阻率油气储集层并非都是泥质砂岩,岩石颗粒细小的或纯净的细粉砂岩也可能形成低电阻率油气储集层,并且粘土的附加导电性也只有在地层水矿化度比较低时,才会成为造成低电阻率的突出因素,事实表明,当地层水矿化度高于大约300000ppm时,即使储集层含有一些粘土矿物,它所产生的附加导电性也是可以忽略的。

Full color, including green quartz, gray quartz, pink quartz, yellow quartz,°×, black quartz, ocean green, red peony, sorghum red, flower wood, yellow wood, white sandstone, siltstone, purple rock, jen brown plate and other varieties.

花色齐全,包括绿石英、灰石英、粉石英、黄石英、白石英、黑石英、海洋绿、牡丹红、高粱红、花木紋、黄木紋、白砂岩、粉砂岩、紫砂岩、仁棕板等品种。

Predepositional ichnocoenosis mainly occurred in thin-bedded fine sandstone, siltstone and silty mudstone, belonging to shallow lacustrine deposits under normal climate condition.

沉积前遗迹群落主要产在属于正常天气下浅湖相薄层状粉、细砂岩和粉砂质泥岩沉积中。

The Middle Devonian Beitashan Formation consists of a series of intermediate-basic volcanic rocks intercalated with more than 100 m thick picritic layer at the bottom, whereas the Middle Devonian Yundukala Fm. is composed of a series of shallow-sea fine-clastic rocks interbedded intermediate rocks and intermediate-basic rocks. The Late Devonian Jiangzierkuduke Fm. includes pyroclastic rocks intercalated with intermediate-basic and intermediate-acid rocks, whereas the Late Carboniferous Batamayineishan Fm. consists chiefly of basalts and basaltic andesites intercalated with tuff, siltstone and carbonaceous shale.

其中中泥盆世北塔山组为一套中基性火山岩,并且底部含有厚度超过100m的苦橄岩;中泥盆世蕴都喀拉组为一套浅海相细碎屑沉积岩夹中性、中基性火山岩;晚泥盆世江孜尔库都克组为火山碎屑岩夹中基性和中酸性火山岩组合;而晚石炭世巴塔玛依内山组以玄武岩和玄武安山岩为主,夹凝灰岩、粉砂岩和炭质页岩。

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