钻石晶体中结构杂质分布与金伯利岩管状钻石电位的比值(以阿尔汉格尔斯克地区和雅库特地区为例)

G. Khachatryan, N. Anashkina
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引用次数: 0

摘要

利用红外光谱对阿尔汉格尔斯克地区12根管道的钻石进行了比较。根据各矿床金刚石中N、H平均值的正相关关系,发现低品位金刚石管晶体中氢的含量相对于Lomonosov和Grib矿床的钻石要高。在结构杂质分布方面,阿尔汉格尔斯克矿床钻石与雅库特钻石不同;这可能是由于比较钻石的来源物质的不同组成和它们生长的热力学条件。结果表明,氢在雅库特和阿尔汉格尔斯克钻石中都是钻石电位的负因素。这可以部分解释为杂质对金刚石晶体生长的阻断作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Ratio of structural impurity distribution in diamond crystals and kimberlite pipe diamond potentiak (case study of Arkhangelsk region and Yakutia)
IR spectroscopy was used to compare diamonds from 12 pipes, Arkhangelsk region. Based on positive correlation between average N and H values in diamonds from various deposits, it was found that crystals from low-grade diamond pipes are relatively enriched in hydrogen compared with diamonds from Lomonosov and Grib deposits. In terms of structural impurity distribution, Arkhangelsk deposit diamonds differ from Yakutian diamonds; it could be due to various composition of compared diamonds’ source matter and thermodynamic conditions of their growth. It is shown that hydrogen is a negative factor of diamond potential in both Yakutian and Arkhangelsk diamonds. This can partly be explained by impuri-ty blocking effect on diamond crystal growth.
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