保加利亚中部罗多彼斯切普拉雷地区Samurski Dol的石柱石晶体结构

IF 0.2 Q4 GEOSCIENCES, MULTIDISCIPLINARY
V. Kostov-Kytin, R. Nikolova, M. Kadiyski, Iliya Dimitrov
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引用次数: 0

摘要

从位于保加利亚中罗多比斯切佩雷附近的Samurski Dol地区的大理石采石场采集的方石样本进行了化学分析和单晶x射线衍射研究。得到的meme值在70 ~ 75之间。所研究样品的晶体结构在I4/m和P42/n两个空间群中都得到了解决,传统上被分配给scapolite成员。本文从硅离子和铝离子的优先位置及其框架排序等方面,对角长石晶体结构的正确空间群的选择提供了新的认识。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Crystal structure of scapolite from Samurski Dol, Chepelare region, Central Rhodopes, Bulgaria
Samples of scapolite from the marble quarry from the Samurski Dol locality, situated nearby Chepelare, Central Rhodopes, Bulgaria have been subjected to chemical analyses and single crystal X-ray diffraction studies. The obtained values for the meionite component (Me) range between 70 and 75. The crystal structure of the studied sample has been solved in both I4/m and P42/n space groups, traditionally assigned to scapolite members. The paper provides new insight on the choice of correct space group for description of scapolites crystal structures, with a view of the preferred positions by silicon and aluminum ions and their framework ordering.
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