首页> 外文OA文献 >A new indicator mineral methodology based on a generic Bi-Pb-Te-S mineral inclusion signature in detrital gold from porphyry and low/intermediate sulfidation epithermal environments in Yukon Territory, Canada
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A new indicator mineral methodology based on a generic Bi-Pb-Te-S mineral inclusion signature in detrital gold from porphyry and low/intermediate sulfidation epithermal environments in Yukon Territory, Canada

机译:基于普通Bi-pb-Te-s矿物包裹体特征的新指示矿物方法,来自斑岩和加拿大育空地区低/中硫化超热环境的碎屑金

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摘要

Porphyry-epithermal and orogenic gold are two of the most important styles of gold-bearing mineralization within orogenic belts. Populations of detrital gold resulting from bulk erosion of such regions may exhibit a compositional continuum wherein Ag, Cu, and Hg in the gold alloy may vary across the full range exhibited by natural gold. This paper describes a new methodology whereby orogenic and porphyry-epithermal gold may be distinguished according to the mineralogy of microscopic inclusions observed within detrital gold particles. A total of 1459 gold grains from hypogene, eluvial, and placer environments around calc-alkaline porphyry deposits in Yukon (Nucleus-Revenue, Casino, Sonora Gulch, and Cyprus-Klaza) have been characterized in terms of their alloy compositions (Au, Ag, Cu, and Hg) and their inclusion mineralogy. Despite differences in the evolution of the different magmatic hydrothermal systems, the gold exhibits a clear Bi-Pb-Te-S mineralogy in the inclusion suite, a signature which is either extremely weak or (most commonly) absent in both Yukon orogenic gold and gold from orogenic settings worldwide. Generic systematic compositional changes in ore mineralogy previously identified across the porphyry-epithermal transition have been identified in the corresponding inclusion suites observed in samples from Yukon. However, the Bi-Te association repeatedly observed in gold from the porphyry mineralization persists into the epithermal environment. Ranges of P-T-X conditions are replicated in the geological environments which define generic styles of mineralization. These parameters influence both gold alloy composition and ore mineralogy, of which inclusion suites are a manifestation. Consequently, we propose that this methodology approach can underpin a widely applicable indicator methodology based on detrital gold.
机译:斑岩表生热金和造山带金是造山带内含金矿化的两种最重要的方式。由这些区域的整体腐蚀所产生的碎屑金的种群可能表现出组成连续体,其中金合金中的Ag,Cu和Hg可能在天然金展现的整个范围内变化。本文介绍了一种新方法,可以根据碎屑金颗粒中观察到的微观夹杂物的矿物学来区分造山和斑岩表生金。在育空地区(核-收入,赌场,索诺拉峡谷和塞浦路斯-克拉扎)钙碱性斑岩矿床周围的近生,斜坡和砂矿环境中共有1459粒金粒已根据其合金成分(Au,Ag ,铜和汞)及其包裹体矿物学。尽管不同岩浆热液系统的演化存在差异,但金在包裹体中仍显示出清晰的Bi-Pb-Te-S矿物学特征,育空造金和金中的特征极弱或(最常见)来自全球造山环境。在育空地区样品中观察到的相应包裹体中,已经确定了以前在斑岩-表热转变过程中发现的矿石矿物学的一般系统组成变化。然而,从斑岩矿化中金中反复观察到的Bi-Te缔合持续存在于超热环境中。 P-T-X条件的范围在定义一般矿化样式的地质环境中被复制。这些参数都会影响金合金的成分和矿石的矿物学,其中包涵体就是一个体现。因此,我们建议这种方法论方法可以为基于碎屑金的广泛适用的指标方法论奠定基础。

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