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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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Detalles Bibliográficos
Autores principales: Williams, Helen M., Matthews, Simon, Rizo, Hanika, Shorttle, Oliver
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2021
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7954453/
https://www.ncbi.nlm.nih.gov/pubmed/33712459
http://dx.doi.org/10.1126/sciadv.abc7394