Looking at the coordinates of the samples they seems to be the same location pretty much if not samples of the same outcrop. Focussed rockchip sampling a little different from 2.5km strike length of thick intersections.
Will be interesting to see how this develops. Posted a link to a paper the other day on WA1 chat about phases of carbonatite melt and how that can concentrate REE's and Nb. So what will be critical is large proportions of host rock enriched rather than thin veins as I think they are referring to here?
All IMO and DYOR.
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