Agoracom

here's abit about the geology...

The Tovshiir project is situated in the basin and range grabens on the eastern flank of the Mongolian craton and is dominated by thrust blocks of Paleozoic aged intrusions and volcanics. The Tovshiir mineralization is focused around a major North East trending thrust fault denoted by a contact between younger diorite bodies and the more extensive granitic host rock. Leakage of mineralizing fluids along this thrust has formed sills of quartz mineralization away form the thrust fault into the host diorite and granites. Mapping suggests the sills of quartz form a stacked sequence away from this fault.