Do i have this right? as the holes head into the alteration zone they are not in the higher conductivity/resistivity zones from the I.p that have been correlating with the better results? Is this ok because it is a different style of mineralization hosted in granodiorite and tonalite? Can u go into some depth on this? When reading the surface sample results from Toro Gordo we can see the best intersections came from that alteration zone
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