Geological-Structural Position and Formation Conditions of Gold-Containing Porphyry Copper Deposits of Mekhmanian Ore-Magmatic System (Lesser Caucasus, Azerbaijan)

Mansurov I. Mamoy, Tahmazova H. Tarana, Sattarzadeh A. Nigar
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Abstract

This article focuses on geological-structural position and formation conditions of gold-containing deposits of Mekhmanian ore-magmatic system (OMS) according to tectonic position of deposits, material composition of ore-bearing and ore-hosting intrusive complexes, specifics of mineral composition, quantity and correlation of main and associated components. There is a new data allowing to estimate formation conditions and matter sources of OMS deposits. Productive mineralization has been determined which occurs by two stages- 1) quartz-molybdenite, quartz-chalcopyrite; 2) quartz-chalcosine-pyrite-chalcopyrite, sphalerite-galena-gold-rare-metal. At first stage concentrators of gold are pyrite and chalcopyrite, and its content is non-uniform, and at second stage gold-containing are represented by galena, sphalerite and also fahl ores and tellurides. We distinguish three gold-bearing associations according to mineral composition of ores, they are- quartz-molybdenite-chalcopyrite, quartz-pyrite-chalcopyrite and quartz-galena-sphalerite.
亚塞拜然小高加索地区梅赫曼尼亚矿-岩浆体系含金斑岩铜矿床地质构造位置及形成条件
本文根据金矿床的构造位置、含矿与容矿侵入杂岩体的物质组成、矿物组成特点、主组分及伴生组分的数量和对比,重点探讨了麦赫曼期矿-岩浆体系(OMS)含金矿床的地质构造位置和形成条件。有一种新的数据可以用来估计OMS沉积物的形成条件和物质来源。确定生产性矿化分两个阶段发生:1)石英辉钼矿、石英黄铜矿;2)石英-硫铁矿-黄铜矿,闪锌矿-方铅矿-金-稀有金属。第一阶段金的富集物为黄铁矿和黄铜矿,其含量不均匀;第二阶段金的富集物为方铅矿、闪锌矿,也有黄铁矿和碲化物。根据矿石的矿物组成划分出3种含金组合,分别为-石英辉钼矿-黄铜矿、石英黄铁矿-黄铜矿和石英方铅矿-闪锌矿。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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