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Archean continental crust formed by magma hybridization and voluminous partial melting
Archean (4.0–2.5 Ga) tonalite–trondhjemite–granodiorite (TTG) terranes represent fragments of Earth’s first continents that formed via high-grade metamorphism and partial melting of hydrated basaltic crust. While a range of geodynamic regimes can explain the production of TTG magmas, the processes b...
Guardat en:
| Publicat a: | Sci Rep |
|---|---|
| Autors principals: | , , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Nature Publishing Group UK
2021
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7933273/ https://ncbi.nlm.nih.gov/pubmed/33664326 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-021-84300-y |
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