Anatectic granites in their source region: A comparison between experiments, thermodynamic modelling and nanogranitoids-Reference-Cited by-同舟云学术

Anatectic granites in their source region: A comparison between experiments, thermodynamic modelling and nanogranitoids

Published:2021-11 Issue: Volume:402-403 Page:106046
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Bartoli Omar,Carvalho Bruna B.

Funder

Università degli Studi di Padova

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference123 articles.

1. Solubility of excess alumina in hydrous granitic melts in equilibrium with peraluminous minerals at 700–800 °C and 200 MPa, and applications of the aluminum saturation index;Acosta-Vigil;Contrib. Mineral. Petrol.,2003

2. Experiments on the kinetics of partial melting of a leucogranite at 200 MPa H2O and 690–800 °C: compositional variability of melts during the onset of H2O-saturated crustal anatexis;Acosta-Vigil;Contrib. Mineral. Petrol.,2006

3. Mechanisms of crustal anatexis: a geochemical study of partially melted metapelitic enclaves and host dacite, SE Spain;Acosta-Vigil;J. Petrol.,2010

4. The Extent of Equilibration between Melt and Residuum during Regional Anatexis and its Implications for Differentiation of the Continental Crust: a Study of Partially Melted Metapelitic Enclaves;Acosta–Vigil;J. Petrol.,2012

5. Primary crustal melt compositions: Insights into the controls, mechanisms and timing of generation from kinetics experiments and melt inclusions;Acosta-Vigil;Lithos,2016

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