GUG to GGI new discovery starts at surfaceFirst have a look at the GGI core....
and now have a look at GUG core...
The mineralized zone was discovered within hole KN18-07, which was testing part of a newly identified 300-metre-wide electromagnetic (EM) conductor outlined in a ground geophysical survey completed by the company in 2017. The 209-metre-long hole cut a 120.6-metre interval of mineralized conglomerate starting at 1.3 metres below surface. Mineralization is hosted in a black (carbon bearing), matrix-supported, polymictic conglomerate with subangular to rounded clasts. Sulphide mineralization consists of predominantly pyrrhotite, lesser pyrite and some variably scattered chalcopyrite occurring as veins, stringers, disseminations, clast replacements, and locally semi-massive and narrow massive accumulations. The black matrix likely also contains appreciable, very fine-grained pyrrhotite as it is magnetic. Local sphalerite occurs in the conglomerate as well as in intercalated siltstone and in a potential barite vein.