If they prove up this folded syncline model through drilling, cascavel could become the side show.
“The ore is characterized by a series of quartz veins associated with strong sulfidation. It is hosted by sericite-chlorite- quartz schist and occurs as concordant and sub discordant set of quartz veins with strong sulfide alteration (Pyrite, Arseno-Pyrite). Hydrothermal alteration is strong and marked by the presence of sericite, green mica, carbonate, sulfides and quartz (Photos). The deposit can be classified as classic Orogenic Gold and is regionally very similar to the Serra Grande Mine deposit (+5Moz), owned by Anglo Gold Ashanti in a Greenstone Belt in the same geological region.”
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If they prove up this folded syncline model through drilling,...
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