帕什基矿床(阿富汗努里斯坦省)伟晶岩中绿柱石的杂质组成

Sergey Skublov, N. Hamdard, M. Ivanov, A. Gavrilchik, V. Stativko
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引用次数: 0

摘要

SIMS 方法(二次离子质谱法)测定了来自帕什基锂矿床伟晶岩(阿富汗努里斯坦省)的绿柱石晶体(海蓝宝石)的杂质成分。对 20 种化学元素(包括卤素和水)的含量进行了 12 次局部测定。与稀有金属海蓝宝石(包括世界其他地区的磷灰石伟晶岩)相比,所研究的绿柱石明显富含大离子亲石元素:锂(约 1100 ppm)、纳(4500 ppm)和钾(300 ppm)。锂辉石绿柱石中的高浓度碱性元素被认为是与绿柱石和其他锂矿物伴生的橄榄石在结晶过程中产生的高潜在碱性的遗传标志。绿柱石的这一众所周知的遗传特征是高产锂伟晶岩的特征,因此,在制定努里斯坦和其他伟晶岩矿区锂伟晶岩的搜索和评估标准方面大有可为。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Impurity composition of beryl from spodumene pegmatites of Pashki deposit (Nuristan province, Afghanistan)
The SIMS method (secondary ions mass-spectrometry) determined the impurity composition of a beryl crystals (aquamarine) from the pegmatites of the Pashki lithium deposit (Nuristan province, Afghanistan). 12 local determinations of the content of 20 chemical elements (including halogens and water) were performed. In comparison with aquamarine from rare metals, including spodumene pegmatites from other regions of the world, the studied beryl is significantly enriched with large ion lithophile elements: Li (about 1100 ppm), Na (4500 ppm) and K (300 ppm). High concentrations of alkaline elements in the beryl of lithium pegmatites are considered as a genetic sign of the high potential of alkalis created during the crystallization of spodumene associated with beryl and other lithium minerals. This well-known genetically determined feature of beryl, characteristic of productive lithium pegmatites, therefore is promising in the development of search and evaluation criteria for lithium pegmatites of Nuristan and other pegmatite provinces.
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