Not really. From the Independent Geo's report in the prospectus:...

Not really.

From the Independent Geo's report in the prospectus:

'Klondyke shear mineralisation is within the fuchsite bearing unit that has associated quartz veinlets. In areas of strong mineralisation these quartz veinlets occur at a high frequency within the silicified shear zone, as parallel bands often showing bounding structures, both down dip and along strike.'

So in the stick of core the green mineral is probably fuchsite (chrome mica), the buff coloured mineral could be ankerite (iron-bearing carbonate) and the pale grey-white veinlets are quartz or quartz-carbonate. The alteration minerals are aligned, defining a strong shear fabric.

Here's hoping there's plenty of gold in it too!