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  1. @Anthro @Ceedave The 4.3 Ga age is from coupled Nd-Sm systems (short and long lived); the mafic rocks do not have zircons. The younger age is from zircons in cross-cutting felsic units. This is the work of Jonathan O'Neil (now at ) mcgillnews.mcgill.ca/s/1762/ne

    en.wikipedia.org/wiki/Nuvvuagi

    Some of the rind remains and is compositionally distinct. Recent work has used triple oxygen to constrain seawater chemistry (sciencedirect.com/science/arti)