克拉斯诺亚尔斯克地区乌德列斯科金锑矿岩矿物学特征及成矿序列

O. V. Alikin, A. V. Chumakov, V. N. Rudashevsky
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引用次数: 0

摘要

本文介绍了乌德瑞斯科矿床金锑矿石及其富集产物的岩相学和矿物学研究成果。对矿石的主要矿物组合进行了表征,揭示了矿石的赋存形态,并对Au、Pd、Ag的分布进行了估计。澄清并补充了成矿序列的共生模式。金赋存的重要矿物形式是含金毒砂和天然金(Au、Ag),以及稀有的金长石AuSb2和锑金(Au、Sb)、钯金(Au、Pd)等金属间化物。贵金属形态的多样性及其与伴生硫化物和非金属矿物关系的分析表明,至少有两个不同的成矿早期和晚期阶段。早期确定了早期石英黄铁矿和晚期黄铁矿两个成矿阶段。晚期形成石英—辉锑矿化、黄铁矿—辉锑矿化—石英矿化、黄铁矿—毒砂—辉锑矿化三个连续阶段。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Mineralogical and Petrographic Features and Mineral Formation Sequence of Gold-Antimony Ores from Udereyskoe Deposit (Krasnoyarsk Region)
The article presents results of petrographic and mineralogical studies of gold-antimony ores of the Udereyskoe deposit and their concentration products. The main mineral associations of ores are characterized, mineral forms of occurrence are revealed, and distribution of Au, Pd, Ag is estimated. The paragenetic scheme of mineral formation sequence was clarified and supplemented. The important mineral forms of gold occurrence are goldbearing arsenopyrite and native gold (Au,Ag), as well as rare aurostibite AuSb2 and intermetallides such as antimony gold (Au,Sb), and palladium gold (Au,Pd). The revealed diversity of forms of noble metals and analysis of their relationships with associating sulfides and nonmetallic minerals indicate at least two contrasting early and late stages of ore genesis. Early quartz-pyrite and late pyrite, which are two stages of mineralization, are determened within the early stage. Three consecutive stages of mineralization are established in the late stage: quartz-stibnite, pyrite-stibnite-quartz, and pyrite-arsenopyrite-stibnite.
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