中乌拉尔Pervomaisko-Verkhoturinskaya地区黑锰矿岩体中镍异常与金-石英成矿作用

A. Motov, Yu. E. Malakh, I. Voropaev
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摘要

在乌拉尔中部Pervomaisko-Verkhoturie地区,在Pervomaisko-Verkhoturie地区的Pervomaisky杂岩(σ ν o2p)的风化氧化泥质岩和黑土岩中发现了安娜金(硫化)石英矿床,并与乌拉尔其他地区的一些由黑土岩-辉锌矿体赋存的金-石英矿床一起,发现了镍含量升高的矿田。富铅锌矿中Au和Ni的空间组合可能是受含金成矿构造位错的部分继承所致。因此,黑锌矿岩体中镍、金富集晕的组合是金石英成矿远景区的有利指示。
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Nickel anomalies and gold-quartz mineralization in dunite-harzburgite massifs of the Pervomaisko-Verkhoturinskaya area, Central Urals
Along with some gold-quartz deposits hosted by dunite-harzburgite massifs elsewhere in the Urals, elevated Ni concentrations were revealed within the ore field of the Anna gold-(sulfide)-quartz deposit localized in weathered oxidized dunites and harzburgites of the Pervomaisky complex (συO2p) in the Pervomaisko-Verkhoturie district of the Central Urals. The spatial association of Au and Ni concentrations in dunites-harzburgites may be attributed to a partial inheritance of Ni-controlling tectonic dislocations by those hosting gold mineralization. Therefore, the combination of halos of Ni and Au concentrations in dunite-harzburgite massifs is a favorable indicator of areas prospective for discovery of goldquartz mineralization.
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