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formation of the Hadean-Eoarchean Acasta crust was finally derived from variable sources, each in age and composition. Combining this outcome with information on the protolith and supply-extraction age yields estimates for the vary of Rb/Sr, and by extension composition, that the supply of these rocks may have had.Three-dimensional evaluation of the morphology and orientation of the constructions within the context of host rock fabrics, mixed with texture-specific analyses of major and hint aspect chemistry, present that the ‘stromatolites’ are extra plausibly interpreted as part of an assemblage of deformation constructions formed in carbonate-altered metasediments long after burial. This highlights an increasing drawback of

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