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Generation of Earth's early continents from a relatively cool Archean mantle

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  • Embargoed (until 1/10/19)

Author(s)

Andrea Piccolo, Richard M. Palin, Boris J.P. Kaus, Richard W. White

School/Research organisations

Abstract

Several lines of evidence suggest that the Archean (4.0 2.5 Ga) mantle was hotter than today's potential temperature (TP) of  1350 ° C. However, the magnitude of such difference is poorly constrained, with TP estimation spanning from 1500 ° C to 1600 ° C during the Meso‐Archean (3.2‐2.8 Ga). Such differences have major implications for the interpreted mechanisms of continental crust generation on the early Earth, as their efficacy is highly sensitive to the TP. Here, we integrate petrological modeling with thermo‐mechanical simulations to understand the dynamics of crust formation during Archean. Our results predict that partial melting of primitive oceanic crust produces felsic melts with geochemical signatures matching those observed in Archean cratons from a mantle TP as low as 1450 ° C thanks to lithospheric‐scale Rayleigh‐Taylor‐type instabilities. These simulations also infer the occurrence of intraplate deformation events that allow an efficient transport of crustal material into the mantle, hydrating it.
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Original languageEnglish
Pages (from-to)1679-1697
JournalGeochemistry, Geophysics, Geosystems
Volume20
Issue number4
Early online date1 Apr 2019
DOIs
Publication statusE-pub ahead of print - 1 Apr 2019

    Research areas

  • Continental crust, Early Earth, Geodynamic modeling

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