"The mineralised trend contains numerous end of hole intersections(p2) from the announcement. I take this to meanin additionto the EOH intersections in the priority assays. What these are will be revealed in due course - deep and or narrow; contiguous with upper grade are all possible"... although any one AC hole can hit blade refusal into something hard, it seems probable that most AC holes drilled to or near the transitional-karst semi-weathered carb, or deeper to fresh. I'm not surprise to see elevated Nb at EOH, either some small transitional interface enrichment, or simply that the fresh carbonatite is mineralised and so some holes will end in mineralisation. Problem is, base of the deep Karst weathering layer is not the shallow HG supergene layer they are looking for and probably need to be competitive...
This example from Mt weld shows how variable the base of the transitional karst zone is, compared to the more consistent supergene ore zone.
"mineralised carbonatite complex thatbroadly follows a magnetic anomaly"Simplistic joining the dots, yellow line, suggests a possible slight cross cutting relationship to the magnetics.Results on the line cutting the core of the magnetic feature will be interesting.A possible interpretation is of a large multi-ring complex with today's results in an outer ring"... having looked at a few carbonatites over the last couple of years, it's clear that no two are exactly alike, and some are really weird shaped complexes. This is because the formation of carb complexes develops over time with often many intrusive/hydrothermal events overlapping... some might be related to magnetite dominant pyroxenite rings, some to less magnetic carbonatite rings, dykes, pipes etc.
Quick google and some came up as 'asymmetrical ring dyke carbonatites' not dissimilar to Green. Maybe the carb intrusion only formed in more dilatational northern area of the complex, maybe there isn;t a southern area of the complex, again because structures and dilation simply directed carb fluids that way in that shape
Below is a simplified description of how ring dykes form in carb complexes in an idealised circular, symmetrical shape, easy to see how half cirlces form, and that the actual carbonatite might cross cut an earlier non-carb magnetic ring dyke...
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