Ann: New Discovery at Karlawinda-CMM.AX, page-7

The interactive 3D presentation of Karlawinda gives some interesting perspectives of the overall project and the southern corridor in particular - in fact any area you choose to focus on. If you haven't already done so it is well worth playing around with this.

Here are some screen shots of the Southern corridor and Frankopan;


Some observations, while apparent from the Announcement, became clearer to me:
The density of drilling in the Southern Corridor (SC) is low.
There are two lines of drilling at the southern end of the SC only one of which appears to show up on the plan view.

Both of the southern drill lines show multiple holes with multiple intersections. It is too early to do much correlation but further drilling will be very interesting to see.
The SC could be a strike extension of the Bibra deposit.
The updip (SE) potential appears closed off on both southern lines.
Depth is probably an issue if the mineralization doesn't reach surface.

Frankopan:


Sparse drilling and deep (+200m) somewhat patchy intersections locally high grade (previous info).
Interesting gaps to the north where mineral zones may be shallower.

Looking around the 3d Presentation some other comments:
The B1 trend doesn't look too impressive to me with scattered intersections seldom being reflected in adjacent holes or drill fences.
The Portrush prospect is not one of the designated views - suggests the model may be missing some recent drilling?
The northern extent of Bibra is probably well constrained.
There has been a fair amount of regional drilling -with long drill traverses/fences.

I am still puzzled by the distribution of mineralization at Karlawinda - so many different zones, good continuity where drill density is adequate. If the Southern Corridor is an extension of Bibra then the strike and dip extent is in excess of 2 and 1 Km respectively. Not likely to be continuous. I keep coming back to Tropicana as a vague model for Karlawinda. Enough musing for tonight.

Have a look at the 3D if interested and come to your own conclusions = DYOR.

GLTAH