Ann: Drill Ready Nickel Sulphide Targets Defined at Jimberlana, page-13

The realisation may be something a little along the lines of, maybe the sulphur rich source rocks have weathered away since everything is falling down the feeder pipe. But if your dyke is the feeder pipe (as all dykes and sills are) then it's a little immaterial. So...what this talk reinforced for me is...in, say, Andover, WIndimurra, Carr Boyd, Narndee, etc, you're looking for the basal contact or feeder structure always (it's a broken record isn't it, always looking for the feeder?)....here, you're in the feeder structure. So...why not explore dykes?

Sill wise...if you un-title Julimar, it's basically a sill running long a BIF/shale sequence in an old sedimentary basin. So that explains where Julimar got all it's mojo. And you can assess, relatively easily I'd think, the prospectivity of all the other prospects in the Western Gneiss Terrane by asking whether they're intruding sediments, or more boring granites and basalts.