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首页> 外文期刊>Doklady Earth Sciences >New data on the composition of jordanite-geocronite Pb-Sb-As sulfosalts at the Berezitovoe deposit (Upper Amur Region, Russia)
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New data on the composition of jordanite-geocronite Pb-Sb-As sulfosalts at the Berezitovoe deposit (Upper Amur Region, Russia)

机译:Berezitovoe矿床(俄罗斯上阿穆尔州)中的约旦石-辉铜矿Pb-Sb-As硫盐组成的新数据

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摘要

New data on the composition of jordanite-geocronite Pb-Sb-As sulfosalts in the vein-disseminated gold ore at the Berezitovoe deposit were provided. Within the studied quartz-sulfide sample, some grains of Pb-Sb-As sulfosalts, uniform in composition and azonal, are drastically different from each other in As and Sb contents forming a quasi-continuous range of solid compounds from jordanite to geocronite. Jordanite-geocronite minerals at the Berezitovoe deposit (relative to the Darasun deposit) are characterized by a higher Pb concentration with a low polymetal total. It is assumed that such typomorphic features of the composition of Pb-Sb-As sulfosalts are indicative of specific formation conditions of gold mineralization in polymetallic ores at the Berezitovoe deposit.
机译:提供了有关Berezitovoe矿床脉状散布的金矿中约旦石-辉石Pb-Sb-As硫盐组成的新数据。在所研究的石英硫化物样品中,一些组成和均一性均匀的Pb-Sb-As硫盐晶粒在As和Sb含量上彼此完全不同,从而形成了从约旦石到斜晶石的近似连续的固体化合物。 Berezitovoe矿床(相对于Darasun矿床)的约旦石-新纪元矿物的特点是Pb浓度较高,多金属总量较低。据推测,Pb-Sb-As硫盐的组成的这种错型特征指示了在Berezitovoe矿床的多金属矿石中金矿化的具体形成条件。

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  • 来源
    《Doklady Earth Sciences》 |2016年第2期|402-407|共6页
  • 作者单位

    Far East Fed Univ, Vladivostok, Russia|Russian Acad Sci, Far East Branch, Far East Geol Inst, Pr Stoletiya 159, Vladivostok 690022, Russia;

    Russian Acad Sci, Far East Branch, Far East Geol Inst, Pr Stoletiya 159, Vladivostok 690022, Russia;

    Russian Acad Sci, Far East Branch, North East Interdisciplinary Res Inst, Ul Portovaya 16, Magadan 685000, Russia;

    Russian Acad Sci, Far East Branch, Far East Geol Inst, Pr Stoletiya 159, Vladivostok 690022, Russia;

    Russian Acad Sci, Far East Branch, Far East Geol Inst, Pr Stoletiya 159, Vladivostok 690022, Russia;

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