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首页> 外文期刊>Data in Brief >Mineralogical dataset of natural zeolites from Lessini Mounts, Northern Italy: Analcime, natrolite, phillipsite and harmotome chemical composition
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Mineralogical dataset of natural zeolites from Lessini Mounts, Northern Italy: Analcime, natrolite, phillipsite and harmotome chemical composition

机译:来自Laysini Mounts的天然沸石的矿物学数据集,意大利北部:肛肠,Natrolite,Phillipsite和单曲化学成分

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This dataset article contains mineralogical and chemical data of some natural zeolites such as analcime, natrolite, phillipsite and harmotome. These minerals were found as secondary phases within vesicles and veins in the basaltic rocks of the Lessini Mounts, Northern Italy. Methods for obtaining the datasets include optical microscopy, X-ray diffraction, scanning electron microscopy and electron probe microanalysis. Analcime forms well-developed, transparent to milky crystals with a typical icositetrahedron habit. The average composition of analcime is calculated as Na13.79Ca0.01K0.03Ba0.03[Al14.28Si33.82O96] 16H2O, with all of the extra-framework sites occupied by sodium. Natrolite usually forms hemispherical aggregates with glassy, colourless to white thin prismatic crystals, which generally radiate from a central point. The average chemical composition of natrolite is Na14.28Ca0.14K0.01[Al15.60Si24.59O80] 16H2O. Crystals of phillipsite-harmotome serie occur in a variety of forms and display a highly variable chemical composition, from almost pure compositions to intermediate values. Phillipsite is more common and its average chemical composition is Ca1.40Na0.29K1.08Ba0.27[Al4.68Si11.28O32] 12H2O, while harmotome is rare and has an average chemical composition of Ca0.97Na0.20K0.36Ba0.91[Al4.60Si11.46O32] 12H2O. The obtained dataset can be used for various purposes: it can be used by other authors to compare morphological features and chemical compositions of similar zeolites crystals discovered in other parts of the world, it can be compared with those obtained from similar geologic environments encouraging studies on hydrothermal processes, and it could represent the starting point for a potential exploration of zeolites from an industrial point of view.
机译:该数据集文章包含一些天然沸石的矿物学和化学数据,如肛肠,Natrolite,紫磷酸盐和单位。这些矿物质被发现是紫杉岩岩石中的囊泡和静脉内的二次阶段,意大利北部的玄武岩岩石中。获得数据集的方法包括光学显微镜,X射线衍射,扫描电子显微镜和电子探针微透析。 Analcime表格发达良好,含有典型的冰水习惯的乳状晶体透明。分析的平均组成是Na13.79Ca0.01K0.03Ba0.03 [Al14.28Si33.82O96] 16H2O,其钠均占据了所有框架。 Natrolite通常用玻璃,无色到白色薄棱柱形晶体形成半球形聚集体,其通常从中心点辐射。 Natrolite的平均化学成分为Na14.28Ca0.14K0.01 [Al15.60Si24.59O80] 16H2O。 Phillipsite-Urmotome Serie的晶体以各种形式发生并显示出高度可变的化学组成,从几乎纯的组合物到中间值。菲利普石是更常见的,其平均化学成分是Ca1.40na0.29k1.08ba0.27 [Al4.68Si11.28O32] 12H2O,而单位是罕见的,并且具有CaO 0.97NA0.20k0.36Ba0.91的平均化学成分。[Al4 .60si11.46o32] 12h2o。所获得的数据集可用于各种目的:其他作者可以使用,以比较世界其他地区所发现的类似沸石晶体的形态特征和化学组成,可以与令人鼓舞的类似地质环境中获得的沸石晶体的化学成分。水热过程,它可以代表来自工业观点的沸石潜在探索的起点。

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