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Visible and 'Invisible' Forms of Gold and Silver in the Crystallization Products of Melts in the Fe-S-Ag-Au System: Experimental Data

机译:Fe-S-Ag-Au系统中熔体结晶产物中金和银的可见和“不可见”形式:实验数据

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摘要

The forms of Au and Ag occurrence in the crystallization products of melts in the Fe-S-Ag-Au system depending on the proportions of Fe/S and Ag/Au have been studied at (Fe + S)/(Ag + Au) = 0.1. It is shown that the S-rich systems with S/Fe = 2 contain Au-Ag sulfides and Au-Ag alloys. The systems depleted in S with S/Fe = 1 contain only Au-Ag alloys. The results of XPS provide evidence for the sulfide and metallic components of Au and Ag among the crystallization products of melts in the system studied at S/Fe = 2 and a metallic component with S/Fe = 1. According to the data of electron microprobe analysis, the content of "invisible" forms of noble metals in pyrite and pyrrhotite is < 0.024 wt % for Au and <0.030 wt % for Ag; the contents of "invisible" Au and Ag in troilites are 0.040 +/- 0.013 wt % Au and 0.079 +/- 0.016 wt % Ag.
机译:在Fe-S-Ag-Au体系中,根据Fe / S和Ag / Au的比例,在熔体结晶产物中Au和Ag的存在形式已被研究为(Fe + S)/(Ag + Au) = 0.1。结果表明,S / Fe = 2的富硫系统包含硫化金-银和金-银合金。 S / Fe = 1的S贫化系统仅包含Au-Ag合金。 XPS的结果为在S / Fe = 2下研究的熔体结晶产物中的Au和Ag的硫化物和金属成分以及在S / Fe = 1下的金属成分提供了证据。根据电子探针数据分析,在黄铁矿和黄铁矿中贵金属的“不可见”形式的含量对于Au <0.024 wt%,对于Ag <0.030 wt%;三叶草中“不可见的” Au和Ag的含量为0.040 +/- 0.013 wt%的Au和0.079 +/- 0.016 wt%的Ag。

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  • 来源
    《Doklady Earth Sciences》 |2017年第2期|636-640|共5页
  • 作者单位

    Russian Acad Sci, Sobolev Inst Geol & Mineral, Siberian Branch, Novosibirsk, Russia|Novosibirsk State Univ, Novosibirsk, Russia;

    Russian Acad Sci, Inst Chem & Chem Technol, Siberian Branch, Krasnoyarsk, Russia;

    Russian Acad Sci, Sobolev Inst Geol & Mineral, Siberian Branch, Novosibirsk, Russia;

    Russian Acad Sci, Sobolev Inst Geol & Mineral, Siberian Branch, Novosibirsk, Russia|Novosibirsk State Univ, Novosibirsk, Russia;

    Russian Acad Sci, Sobolev Inst Geol & Mineral, Siberian Branch, Novosibirsk, Russia|Novosibirsk State Univ, Novosibirsk, Russia;

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