RE: RNS1 Oct 2024 11:01
My Mate ChatGPT again. Cut and paste statements from the RNS and ask away.
"Based on the description provided, the gold mineralization described appears to be characteristic of a stockwork assemblage 5 . A stockwork is a network of interconnected veinlets and small-scale fractures that contain mineralization and is commonly associated with hydrothermal systems 5 . The presence of high-grade, sulphide-rich quartz veins and veinlets within or at the contact with an intensely altered felsic unit, as well as the pervasive, lower grade gold mineralization in wide envelopes, aligns with the typical characteristics of a stockwork assemblage commonly found in hydrothermal environments.
Given the presence of such mineralization, it is likely that further exploration and analysis may reveal the potential presence of an underlying mineralized system, such as a deeper-seated epithermal or mesothermal deposit, related to the same hydrothermal activity that formed the stockwork 6 . This deeper-seated mineralization may be associated with a primary source of the mineralizing fluids, potentially leading to the discovery of higher-grade mineralization at depth. Therefore, additional exploration, including drilling and geophysical surveys, may be warranted to assess the potential for deeper mineralized zones beneath the known stockwork assemblage."
What we have is a sizeable surface expression of some significance (IMHO). Some elements have sulfidization which may create a challenge for extraction in these zones however again the widths are significant. This hasn't been drilled yet. Grades look very likley to improve with depth if there is an adjacent source of the mineralisation (of the stockwork zone) then we might be in for a treat. The drill will tell us.
One further point of note is that we are seeing mineable grades in breadth at surface. Very easy to open pit this. Remember too that MBT007 and 008 are 200m apart. In other words we have only just scratched the surface here.
GLA DYOR