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Monday, 07/22/2019 1:18:06 PM

Monday, July 22, 2019 1:18:06 PM

Post# of 244
Throughout the concession areas gold mineralization appears to have strong structural controls, concentrating along lithological contacts and structural breaks. Two styles of gold mineralization have been observed: A pyrite-rich massive sulphide sitting at the contact of a deformed mafic volcano-sedimentary sequence and a thick black shale unit. The massive sulphide is reported to host a drill intercept of 9 meters at 7.6 grams-per-tonne (“g/t”) gold (“Au”)** and is gold-arsenopyrite bearing quartz veins hosted on lithological contacts and within shear zones which assayed between 2 g/t to 7 g/t Au**.

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