Explaining above, There is possibility for LUR002 to have more supergene, but i think they have hit it, and the Oxide/Supergene looks to be transitional between many layers of oxidation as multiple thin supergene.
LURC003 should have more supergene to report, and its interesting that the TREO is very low in LURC003, which mean i think its more primary rock and less weathered as it is on the side of the anomoly. but the background Nb2O5 is actually higher, like PARC003 (P2).
I suspect LURC001 will be the best supergene of all, with a higher near surface anomaly of all holes.
Ann: West Arunta Project - High Grade Nb-Ta in Weathered Zone, page-281
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