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为了更加充分利用南乌拉尔铜矿中的多种元素,弄清金的分布规律是有重要实际意义的.本文以盖依铜矿、南盖依铜矿、塞巴依铜矿、莫洛焦日铜矿等矿区为例,阐述这类矿床中金的一些分布特征.彼得洛夫斯基和普舍尼契尼曾通过他们的研究工作,划分出三个共生矿物组合,即:(1)早期的,为杂有细粒黄铜矿矿物的黄铁矿矿石和杂有细粒黝铜矿、闪锌矿、重结晶的粗粒黄铁矿和黄铜矿的黄铜矿矿石;(2)晚期的,为黄铁矿-黄铜矿-闪锌矿矿石,含黝铜矿的闪锌矿-方铅矿矿石,黄铁矿-斑铜矿矿石;(3)末期的,为石英、碳酸盐、重晶石、纯闪锌矿、
In order to make full use of the various elements in the South Ural copper mine, it is of important practical significance to find out the distribution law of gold.In this paper, the Geyiyan copper deposit, Copper and other mines as an example to illustrate some of the gold distribution characteristics of these deposits Petrovsky and Pronouachenny, through their research work, divided three symbiotic mineral assemblages, namely: (1) early , Pyrite ores with fine-grained chalcopyrite minerals and chalcopyrite ores with chalcopyrite, sphalerite, recrystallized coarse-grained pyrite and chalcopyrite; (2) In the late stage, they are pyrite-chalcopyrite-sphalerite ore, sphalerite-containing galena-galena ore and pyrite-bornite deposits; (3) Acid salt, barite, pure sphalerite,