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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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| Publicado en: | Sci Adv |
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| Main Authors: | , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado: |
American Association for the Advancement of Science
2021
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| Assuntos: | |
| Acceso en liña: | 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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