I am watching it like a hawk and will certainly buy if the drilling results are good enough to suggest a potential economic gold discovery.
But you are not a structural geologist are you, from what you say below. I wouldn't use the word likely:
The veins set at Thylacine looks like a simple 'Riedel' fracture system, orientated WNW-ESE, within in a localised dextral shear.
Thir regular repetition and similar orientation and width is a function of the stress field at the time, which formed them, the rheological properties of the **broic rock that they formed in.
The individual veins are unlikely to have much 'along strike' continuity beyond the enclosing shear in a NW-SE direction. They will be confined by the boundaries of this enclosing shear envelope (in red below).
The overall WNW-SSE vein envelope may continue further at either end, and there may be additional veins under cover there, if there is any cover to hide them.
These seem unlikely to be any thicker than the 0.2m to 1.0m thickness of the known outcropping veins mapped and described by the company. Particularly so as the individual veins at Thylacine run parallel to the original Siberian Tiger vein, have formed in the same stress field, and are of a similar width to Siberian Tiger. But again, well worth drilling these extensional areas just in case.
Thylacine: a WNW-ESE dextral shear zone (red) enclosing a set of NW-SE Riedel fractures (yellow)
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