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chlorite相关的网络例句

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与 chlorite 相关的网络例句 [注:此内容来源于网络,仅供参考]

Wall-rock alteration green color stone, mainly composed of hoepfnerite, epidote, diopside, biotite, quartz, and chlorite etc.

富矿体两侧发育流体交代岩,这些绿色岩石是块状富矿体和角砾状富矿体的主要容矿岩石,这与热水沉积形成的层纹状锌矿具有显著差异。

In accordance with the process, the hydroxy carboxylic acid serves to temporarily transfer chlorine from and does not form a salt with the alkali metal salt of a chlorite ion.

根据本方法。羟基羧酸用作暂时转移氯,并且与亚氯酸根离子的碱金属盐不生成盐。

A method for forming an aqueous chlorine dioxide solution is disclosed which includes reacting in a reaction vessel an acid reaction solution containing a hydroxy carboxylic acid and a companion acid with an alkali metal salt of a chlorite ion.

本发明公开了一种生成含水的二氧化氯溶液的方法,其中包括在反应容器中让含有羟基羧酸和配对酸的酸的反应溶液与亚氯酸根离子的碱金属盐进行反应。

According to a Material Safety Data Sheet published by Elmers Products, Inc. this material includes an acrylic binding resin and 5 to 10% by weight magnesium carbonate, 50 to 70% limestone, 1 to 5% chlorite, 1 to 5% kaolin, 1 to 5% calcite, 5 to 10% talc and 0.1 to 0.99% quartz.

根据材料安全数据表Elmers出版的产品,公司这种材料包括丙烯酸树脂和具有约束力的5至10 %的重量碳酸镁, 50至70 %,石灰石, 1至5%,绿泥石, 1至5 %高岭土, 1至5%,方解石, 5至10 %,滑石粉和0.1至0.99 %石英。

The results showed that the major components of the solid particles were α-Quartz、Illite、Chlorite、Montmorillonite、Albite、Microcline、Kaolinite and Calcite.

研究表明:长江口水体固相颗粒质中主要含有下列矿物成分:石英、伊利石、绿泥石、蒙托石、钠长石、钾长石、高岭石和方解石。

Plagioclase and potassic feldspar had experienced serious alteration in both core and rind in monzonite, and pyroxene had changed to chlorite in rind with thin section analysis.

薄片鉴定发现二长岩核心及外环的斜长石及钾长石均发生了强烈风化,外环中的辉石变为绿泥石。

From altered mylonite to altered untramylonite, the crystallinity of illite decreases whereas that of chlorite shows no obvious variation with the increasing strain.

由应变较弱的蚀变糜棱岩带到应变较强的蚀变超糜棱岩带,伊利石的结晶度有变小的趋势,而绿泥石的结晶度则基本保持不变。

The temperatures obtained using the muscovite-biotite geothermometer and chlorite compositional geothermometer range between 672℃ and 1116 ℃ and between 470℃and 520 ℃ respectively, being higher than the deformation temperatures of mylonites in the ductile shear zone, which suggests that the two geothermometers are not applicable to calculation of the formation temperatures of low-temperature mylonite.

利用白云母-黑云母地质温度计和绿泥石地质温度计获得的温度值分别为672 ℃~1 116 ℃和470 ℃~520 ℃,高于糜棱岩的形成温度,指示这2个地质温度计不适用于计算低温糜棱岩的形成温度。

There exist strong negative correlation between crystal size and crystallinity of illite in altered mylonite of low strain and low water/rocks ratios, and positive correlation between crystal size and crystallinity of chlorite in altered untramylonite of high strain and high water/rocks ratios.

在岩石应变较弱、水/岩比较小的糜棱岩带,伊利石的平均结晶大小与结晶度成负相关,而在岩石应变较强、水/岩比较大的超糜棱岩带,绿泥石的平均结晶大小与结晶度成正相关。

In this paper an attempt is first made to apply the above-mentioned three geothermometers in mylonite by using syn-tectonic neogenic muscovite, biotite and chlorite of mylonites in a ductile shear zone in the southern segment of the Tanlu fault zone.

本文利用郯庐断裂带南段韧性剪切带内糜棱岩中同构造新生的白云母,黑云母和绿泥石,首次尝试上述3种地质温度计在糜棱岩中的应用。

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