Ann: Strong Sulphidic Lodes Intersected at Rebecca, page-18

"Preliminary geological logging of RHD04 has confirmed four zones of significant disseminated (+/- matrix style) pyrrhotite, pyrite and traces of chalcopyrite mineralisation in silica+/-sericite altered gneiss, each with downhole widths of between 8m and 18m. "

These guys sure say what they mean, and mean what they say..

I appreciate the posters above who translate these announcements - it's why I like this forum.

Some Luddite questions please: Is this the same type of mineralisation associated with the previous good results? Can anyone hazard a guess to what success looks like in regard to upcoming assays? And how long will the lab take to return this information?


Silica+/-sericite altered gneiss to you all.