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Abstract

Recent exploration work by Société Minière Sphinx has exposed significant gold mineralization in a quartz vein system hosted by highly carbonatized mafic metavolcanics. A vast area of stripped outcrop permits the observation of severa1 fundamenta1 characteristics of Archean go1d-bearing hydrotherma1 systems. During this visit, several of these characteristics that document the evolution of the hydrothermal system will be examined.

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