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Noble-metal mineralization of the Adycha-Taryn metallogenic zone: geochemistry of stable isotopes, fluid regime, and ore formation conditions

机译:AdyCha-Taryn Metallenic区的贵金属矿化:稳定同位素,流体制度和矿石形成条件的地球化学

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摘要

The regional geologic setting of the Adycha-Taryn metallogenic zone, one of the areas most productive for noble-metal mineralization in northeastern Russia, is discussed. The intricate metallogenic history of the zone and the prolonged geodynamic activity of its ore-hosting structures are documented. Different types of mineralization, such as hydrothermal-metamorphogenic, gold-bismuth, gold-quartz, gold-antimony, and silver-antimony, are described. New data on the isotopic compositions of oxygen in quartz, sulfur in sulfides, and oxygen and carbon in carbonates from different mineralization types are presented. The early metamorphogenic quartz beyond the ore zones has delta O-18 = +20.1 +/- 2.0 parts per thousand. At the gold-bismuth deposits, the delta O-18 values of quartz are within the narrow range of +12.5 +/- 0.4 parts per thousand. Quartz from the gold-quartz mineralization shows much wider variation in delta O-18 values, from +14.2 to +19.5 parts per thousand. A similar range (delta O-18 = +16.1 to +19.2 parts per thousand) is observed for the gold-antimony mineralization. Crzptograined quartz from the silver-antimony mineralization is enriched in light oxygen isotopes (delta O-18 = -3.2 to +4.7 parts per thousand). The following delta S-34 values (parts per thousand) have been established in sulfides of mineralization of different types: gold-bismuth -3.7 to -2.2 (Apy) and -6.7 to -6.8 (Py); gold-quartz -2.1 to +2.4 (Apy), -6.6 to +5.4 (Py), and -6.1 to +4.2 (St); gold-antimony -2.0 to +1.6 (Apy), -3.5 to +2.1 (Py), and -5.3 to +0.2 (St); and silver-antimony -2.0 to -1.9 (Apy), -2.2 +/- 0.1 (Py), and -5.7 to -5.6 (St). The delta C-13 and delta O-18 values are contrasting in the studied types of mineralization, varying respectively from -6.9 to -5.9 parts per thousand and from +2.1 to +5.7 parts per thousand (gold-bismuth), from -9.1 to -6.1 parts per thousand and from +12.4 to 18.7 parts per thousand (gold-quartz), from -12.1 to -9.5 parts per thousand and
机译:讨论了俄罗斯东北部贵金属矿化最富含贵金属矿化的地区地质环境。记录了该区域的复杂成矿历史和其矿物宿主结构的延长的地球动力学活性。描述了不同类型的矿化,如热炎麦白发生,金 - 铋,金石英,金锑和银锑。提出了关于石英,硫酸硫中氧同位素组成的新数据,以及来自不同矿化类型的碳酸盐中的氧气和碳酸盐。矿石区外的早期型晶晶石英具有Delta O-18 = +20.1 +/- 2.0份。在金 - 铋沉积物上,石英的Delta O-18值在左幅的范围内+12.5 +/- 0.4份。来自金石英矿化的石英显示了ΔO-18值的更广泛的变化,从+14.2到+19.5份。对于金锑矿化,观察到类似的范围(Delta O-18 = +19.2 + +19.2份)。来自银锑矿化的Crzptogromgregreg矿化在轻氧同位素(Delta O-18 = -3.2至+ 4.7份/份每千份)中富集。已经在不同类型的矿化中建立了以下ΔS-34值(千分比):金 - Biscuth -3.7至-2.2(APY)和-6.7至-6.8(PY);金 - Quartz -2.1至+2.4(APY),-6.6至+5.4(PY)和-6.1至+4.2(ST);金 - 锑-2.0至+1.6(APY),-3.5至+2.1(PY),和-5.3至+0.2(ST);和银锑-2.0至-1.9(apy),-2.2 +/- 0.1(py),和-5.7至-5.6(st)。 ΔC-13和Delta O-18值在研究的矿化类型中对比,分别从-6.9至-5.9份,从-9.1分别从-6.9至-5.9份,从+ 2.1到+ 5.7份(金 - 铋),从-9.1分别每千千分之千至6.1分,从+12.4至18.7份(金石英),从-12.1到-9.5份千分之一

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