The geology of the Vuzel gold project is dominated by a district Palaeogene sintectonic sedimentary basin within and above the metamorphic basement. That basin is controlled by east-west and northwest post collisional extensional faults and is filled by sedimentary rocks of the Kroumovgrad, breccia-conglomerate and coal bearing sandstone-conglomerate units. These sedimentary units are the predominant host of the outlined Vuzel epithermal gold mineralisation.
RDN Price at posting:
0.5¢ Sentiment: Sell Disclosure: Not Held
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