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No evidence for high-pressure melting of Earth’s crust in the Archean
Much of the present-day volume of Earth’s continental crust had formed by the end of the Archean Eon, 2.5 billion years ago, through the conversion of basaltic (mafic) crust into sodic granite of tonalite, trondhjemite and granodiorite (TTG) composition. Distinctive chemical signatures in a small pr...
Αποθηκεύτηκε σε:
| Τόπος έκδοσης: | Nat Commun |
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| Κύριοι συγγραφείς: | , , , , , , , , , , , |
| Μορφή: | Artigo |
| Γλώσσα: | Inglês |
| Έκδοση: |
Nature Publishing Group UK
2019
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| Θέματα: | |
| Διαθέσιμο Online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6895241/ https://ncbi.nlm.nih.gov/pubmed/31804503 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-019-13547-x |
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