罗马尼亚阿普塞尼山脉比霍尔成矿带五元素矿化中并存的二砷化镍多晶体

G. Săbău, George Dincă, Andra-Elena Filiuță
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摘要

在比霍尔金属成因区的五元素矿化物中,发现了三种已知的二砷化镍多晶体以明显的平衡状态共存。这是在罗马尼亚首次发现pararammelsbergite和krutovite,该矿区也是所有三种NiAs2多晶体共存的极少数矿点之一。在罗马尼亚新发现的这两种物相都很容易通过光学特性与雷姆贝里石区分开来,并在化学计量和同构取代程度上显示出一致的成分差异。NiAs2 多晶体与镍线石和矽卡岩共存,在中温沉积序列中明显早于钴铁-格氏钴铁矿,其特征是金属-贫砷化物中的镍和钴最初分离,随后砷活性持续降低,硫活性增加,镍线石模态增加,格氏钴铁矿-钴铁矿系列中的钴富集。
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Coexisting nickel diarsenide polymorphs in the five-element mineralization of the Bihor metallogenetic district, Apuseni Mountains, Romania
The three known polymorphs of nickel diarsenide were found to coexist in apparent equilibrium in the five-element mineralizations of the Bihor Metallogenetic District. It is the first identification of pararammelsbergite and krutovite in Romania, and the locality joins a very limited list of occurrences where all three NiAs2 polymorphs coexist. Both phases newly identified in Romania are easily distinguishable from rammelsbergite by their optical properties and display consistent compositional differences manifested in stoichiometry and degree of isomorphic substitution. The NiAs2 polymorphs coexist with nickeline and skutterudite and apparently predate cobaltite-gersdorffite in a mesothermal depositional sequence characterized by initial separation of Ni and Co in metal-poorer arsenides, followed by continuous decrease of arsenic activity, increase in sulfur activity, modal increase of nickeline and Co enrichment in the gersdorffite-cobaltite series.
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