Investor Presentaiton slide image

Investor Presentaiton

OURCES ING Drone-based Magnetics At Omu sinter, a plot of residual intensity profound magnetic shows a north- northeast trending zone of low magnetism (blue) where alteration hydrothermal has obliterated traces of magnetite in volcanic rocks. Irving views this zone as a robust target prospective for high- grade epithermal vein mineralization. Note, this zone is coincident with a prominent gravity gradient highlighting a graben-bounding fault underlying this area (upper left). Oma Sinter 1km Omu Sinter IRV:CNX 21 27
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