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Iron isotopes trace primordial magma ocean cumulates melting in Earth’s upper mantle

The differentiation of Earth ~4.5 billion years (Ga) ago is believed to have culminated in magma ocean crystallization, crystal-liquid separation, and the formation of mineralogically distinct mantle reservoirs. However, the magma ocean model remains difficult to validate because of the scarcity of...

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Publicat a:Sci Adv
Autors principals: Williams, Helen M., Matthews, Simon, Rizo, Hanika, Shorttle, Oliver
Format: Artigo
Idioma:Inglês
Publicat: American Association for the Advancement of Science 2021
Matèries:
Accés en línia:https://ncbi.nlm.nih.gov/pmc/articles/PMC7954453/
https://ncbi.nlm.nih.gov/pubmed/33712459
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.abc7394
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