Too early to say anything about what's orientated where. Perpendicular allows for a full 360 degrees of rotation. I'll just take it to mean not parallel.
Not as likely to be replacement of strataform carbonates given a non-conforming orientation. Shear hosted fracture filling with carbonates precipitated from metamorphic fluids. Looks like the copper and silver in very close association presumably originally as sulphides, and the tungsten probably separate to some degree, probably as scheelite.
The "discovery" story is all backwards due to the nature of it. You would normally get a discovery hole and then go from there. Not just fluke one out of a heap drilled for other purposes and then have a bunch of maybes within them. Anyway - it's still a discovery, and they are funded to drill it. Nothing is ever as simple as one may wish.
We'll see how they go.
OGX Price at posting:
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