Crustal rejuvenation stabilised Earth’s first cratons

Why Earth’s crust only started becoming widely preserved in the Eoarchaean, 500 Ma after planetary accretion, is poorly understood. Here, the authors document a shift to juvenile magmatic sources in the early Eoarchaean, linking crustal preservation to the formation of stabilising melt-depleted mant...

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Autores principales: Jacob A. Mulder, Oliver Nebel, Nicholas J. Gardiner, Peter A. Cawood, Ashlea N. Wainwright, Timothy J. Ivanic
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/9eb8dac0d30f42fca495de4915f7a9d1
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