Speculative Guesstimate #1, page-2

There is a catch 22 herelike VTM, if the carbonatite/alkaline REE is soluble which it maybe very well be, then the carbonatite maybe Barron of REE as it has dispersed to a massive ring around the area. However this potentially makes the REE in "clay pot" regolith easier to process, We already know for historical samples and rock chips that the phosphorus carbonatite area has grades up to 1200ppm 2Reo+Y by memory If this is a VTM type deposit, which I think the more I look it actually could be, then it's great, just need size, grade and proof of ionic extraction. The 4.6% means there could be so hydrothermal dyke veins like lofdal Namibia, which could increase resource significantly but not be ionic. The 4.6% has not spread. They missed it be 5m but may have been redrilled in 50 hole program one thing that stood out to me is that the HREE are transported further away from the potential source, where yttrium is high concentration towards the source, just like VTM