Bro
@Hateful8 , Im trying to understand the previous CDE assays and how could they get up to 1600g/m and the high grade mineralisation is very near surface. So far we have identified 14 high grade faults, a few of them for example CC450, had higher grade than the others. But to reach a grade of 1600g/m (assuming that the CDE assay is still reliable) I think there could only be 2 scenarios: they hit where the faults are joining or different faults system with greater thickness.
Bro
@mach8 also tried to locate the previous CDE holes and put them on the current drilling campaign map:
According to his map, the light blue dots (previous CDE holes) are located more to the East of the known faults. And when I look to the overall map below, I can make sense out of it because it seems like some faults are joining Easternly, may be thats where CDE hit them?
But in your map, it seems like the CDE holes are towards Toro Gordo? So how can we explain the high grade? Different faults system? Or the faults are joining there instead?
Too bad the IP survey is too narrow so we dont know what's going on Southernly and Easternly to confirm our theory.
@Hateful8@mach8@123david321 what are your opinions on this?
