Coexisting bournonite-seligmanite and tennantite-tetrahedrite solid solutions in Darasun gold deposit (Eastern Transbaikalia, Russia): Estimation of the mineral formation temperature

N. Lyubimtseva, N. Bortnikov, S. E. Borisovsky
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Abstract

Mineral associations, intergrowth features, chemical composition and Sb and As distribution in coexisting fahlore and bournonite-seligmanite solid solutions in the Darasun gold deposit were studied. For the first time the almost complete solid solution was found between bournonite and seligmanite with a continuous isomorphism between Sb and As in the range of Sb/(Sb + As) ratios from 0.21 to 1.00 in the Darasun deposit by EMPA. The composition of the fahlore coexisting with bournonite varies widely: Sb/(Sb + As) ratios 0.03-0.96 and Fe/(Fe + Zn) ratios 0.36-0.87. The coupled compositional evolution from early antimony to late arsenic in coexisting solid solutions has been established. Based on the investigation of the Sb and As distribution between coexisting fahlore and bournonite-seligmanite, the temperatures of their joint deposition and, as a result, of the productive stage, in which they are closely associated with native gold and tellurides (90–335 °С), are estimated.
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俄罗斯东外贝加尔达拉森金矿床中硼辉石-矽辉石和钛辉石-四面体共存固溶体:矿物形成温度的估算
研究了大孙金矿区辉钼矿和铌铁钨矿共存固溶体中的矿物组合、共生特征、化学组成及Sb、As的分布。经EMPA分析,首次发现大拉孙矿床中布菱矿与铁长石之间存在几乎完全的固溶体,且Sb与As在Sb/(Sb + As)比值0.21 ~ 1.00范围内呈连续同形。与bournonite共存的fahore组成差异很大,Sb/(Sb + As)比值为0.03 ~ 0.96,Fe/(Fe + Zn)比值为0.36 ~ 0.87。建立了共存固溶体中从早期锑到晚期砷的耦合组成演化。通过对共生辉钼矿和铌铁-铁长石之间的Sb和As分布的研究,估计了它们的节理沉积温度,以及它们与天然金和碲密切相关的生产阶段温度(90-335°С)。
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