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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...

Disgrifiad llawn

Wedi'i Gadw mewn:
Manylion Llyfryddiaeth
Cyhoeddwyd yn:Philos Trans A Math Phys Eng Sci
Prif Awduron: Nebel, O., Capitanio, F. A., Moyen, J.-F., Weinberg, R. F., Clos, F., Nebel-Jacobsen, Y. J., Cawood, P. A.
Fformat: Artigo
Iaith:Inglês
Cyhoeddwyd: The Royal Society Publishing 2018
Pynciau:
Mynediad Ar-lein:https://ncbi.nlm.nih.gov/pmc/articles/PMC6189554/
https://ncbi.nlm.nih.gov/pubmed/30275165
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rsta.2018.0103
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