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...

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Detalles Bibliográficos
Autores principales: Hernández-Montenegro, Juan David, Palin, Richard M., Zuluaga, Carlos A., Hernández-Uribe, David
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7933273/
https://www.ncbi.nlm.nih.gov/pubmed/33664326
http://dx.doi.org/10.1038/s41598-021-84300-y

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7933273/
https://www.ncbi.nlm.nih.gov/pubmed/33664326
http://dx.doi.org/10.1038/s41598-021-84300-y

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