首页> 外文期刊>Mineralium deposita >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:一种新的指标矿物方法,基于斑岩和低/中级硫化岩体岩体岩土覆盖岩体岩土的仿制黄金矿物包裹型血管术中的矿物质方法。加拿大

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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:斑岩膜和造口黄金是造口带中最重要的粘矿矿化风格。堆积金的填充金的堆积可能表现出一种组合物连续体,其中金合金中的Ag,Cu和Hg可以随天然金而呈现的全部范围变化。本文描述了一种新的方法,可以根据在滴乳金颗粒内观察到的微观夹杂物的矿物质的矿物学和斑岩骨骺金。在育空(Nucleus-Gente,Casino,Sonora Gulch和Cyprus-Klaza)的钙碱性斑岩沉积物周围共有1459粒的黄金谷物,在其合金组合物(Au,Ag ,Cu和Hg)及其包涵体矿物学。尽管不同岩浆水热系统的演化存在差异,但黄金在含有套件中表现出清晰的双PB-TE-S矿物质,其签名或(最常见的)在Yukon Orogenic Gold和Gold中缺席来自全球organic的环境。在从育空中的样品中观察到的相应的含有套件中,已经鉴定了先前鉴定过斑岩覆膜过渡的矿石矿物的通用系统成分变化。然而,从斑岩矿化的黄金中反复观察到的BI-TE协会仍然存在于骨骺内。 P-T-X条件的范围在地质环境中复制,这些环境定义了矿化的通用风格。这些参数影响金合金组合物和矿石矿物质,其中包含套件是表现形式。因此,我们提出这种方法方法可以基于碎屑金提供广泛适用的指标方法。

著录项

  • 来源
    《Mineralium deposita》 |2018年第6期|共20页
  • 作者单位

    Univ Leeds Sch Earth &

    Environm Leeds Ores &

    Mineralizat Grp Leeds LS2 9JT W Yorkshire England;

    Univ British Columbia Dept Earth Ocean &

    Atmospher Sci Mineral Deposit Res Unit 2020-2207 Main Mall Vancouver BC V6T 1Z4 Canada;

    Univ British Columbia Dept Earth Ocean &

    Atmospher Sci Mineral Deposit Res Unit 2020-2207 Main Mall Vancouver BC V6T 1Z4 Canada;

    Radius Gold Suite 650 200 Burrard St Vancouver BC V6C 3L6 Canada;

    Univ Leeds Sch Earth &

    Environm Leeds Ores &

    Mineralizat Grp Leeds LS2 9JT W Yorkshire England;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 矿床学;
  • 关键词

    Gold; Indicator mineral; Microchemical characterization; Porphyry systems;

    机译:金;指标矿物质;微型化学表征;斑岩系统;

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