Rcrust: a tool for calculating path-dependent open system processes and application to melt loss

Earth's continental crust is stabilized by crustal differentiation that is driven by partial melting and melt loss: Magmas segregate from their residuum and migrate into the upper crust, leaving the deep crust refractory. Thus, compositional change is an integral part of the metamorphic evoluti...

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Veröffentlicht in:	Journal of metamorphic geology 2016-09, Vol.34 (7), p.663-682
Hauptverfasser:	Mayne, M. J., Moyen, J.-F., Stevens, G., Kaislaniemi, L.
Format:	Artikel
Sprache:	eng
Schlagworte:	anatexis Basins Closed systems Continental crust decompression melting Earth Sciences Geochemistry melt loss Open systems Rcrust Sciences of the Universe thermodynamic modelling
Online-Zugang:	Volltext
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