When crust comes of age: on the chemical evolution of Archaean, felsic continental crust by crustal drip tectonics

The secular evolution of the Earth's crust is marked by a profound change in average crustal chemistry between 3.2 and 2.5 Ga. A key marker for this change is the transition from Archaean sodic granitoid intrusions of the tonalite–trondhjemite–granodiorite (TTG) series to potassic (K) granitic...

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Detalles Bibliográficos
Autores principales: Nebel, O., Capitanio, F. A., Moyen, J.-F., Weinberg, R. F., Clos, F., Nebel-Jacobsen, Y. J., Cawood, P. A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: The Royal Society Publishing 2018
Materias:
Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6189554/
https://www.ncbi.nlm.nih.gov/pubmed/30275165
http://dx.doi.org/10.1098/rsta.2018.0103

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6189554/
https://www.ncbi.nlm.nih.gov/pubmed/30275165
http://dx.doi.org/10.1098/rsta.2018.0103

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