Ann: Further impressive thick and high grade gold at Hemi, page-94

Thanks for the points Lethal, and I’m happy to be of the same thinking as it gives the area more potential.
I still thought there was potential for A and B to join up because as you said there’s enough space for it. I just wasn’t keen about section C from where it was placed. ie lode would be boomerang shaped , but if Andy is postulating a A to C , and a B to the S/W intrusive , that works well. It keeps the same alignment as the other intrusives in the region which conform to the Antwerp Trend. ( my black arrows- trend?)
My initial reasoning was the Hemi intrusive ‘ seemed’ to align differently to others in the region as shown on the DEG plan map.


My speculative punt was a cross cutting fault at depth like is shown in regional mapping ( below). Though they seem to be confined to deformation events to the south and west of the Mallina Basin, not secondary faults, and that I think the basin is in extension and compression ( squeezing and lengthening).
I suppose the Hemi intrusives here are just a funny shaped blobs and not relevant.
What is relevant is the the Mallina shear zone is the major shear in Pilbara Craton, is very old 3.0 Ga ,very deep roots , and has has multiple deformation events, these sanukitoid intrusions being an example.
And of course that they’re in very early exploration stages.