RE: 1st post/investment27 Jan 2021 16:51
I'll check that post out AGEOS. So far from what i've read of the tech report and your posts, plus my general knowledge of Colombia etc, that epithermal overprint of VMS is exactly my hypothesis right now. Given the tectonic setting, the VMS would be a back-arc environment which would support the Kuroko type analogy they refer to in the tech report. This would be Cretaceous age. Then as the subduction zone develops and more accretions occur, we get the Neogene aged porphyries/epithermal systems start to come about. We know we have Miocene age intrusions nearby. Therefore not only can the younger intrusions generate epithermal veins etc, the hydrothermal system could remobilise pre-existing mineralization. Therefore if the VMS was originally a gold rich VMS, it's possible that gets remobilised to an extent. However as you probably know, this would need a serious amount of drilling/investigation to verify likely in conjunction with some university analytical equipment. Best to take things one stage at a time but i'm quite confident this system has an epithermal component to it
Cheers
Magic