Ok, i did some reading for you nammuldi and others, see attached pics:
So now its opposite of what I said below, and in which they (RR1) have corrected themselves in dot point 1, and in the last paragraph of page 1. They are now saying initial thoughts back in may were that it was from a pegametite source, now they are confirming its from a carbonatite source (YAY !!!).
Ann: Fine Grained Alkaline Igneous Host of High Grade Nb/REE, page-19
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