Chemical diffusion of major components in granitic liquids: Implications for the rates of homogenization of crustal melts
Author:
Publisher
Elsevier BV
Subject
Geochemistry and Petrology,Geology
Reference76 articles.
1. Dissolution of corundum and andalusite in H2O-saturated haplogranitic melts at 800°C and 200 MPa: constraints on diffusivities and the generation of peraluminous melts;Acosta-Vigil;Journal of Petrology,2002
2. 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;Contributions to Mineralogy and Petrology,2003
3. Contrasting interactions of sodium and potassium with H2O in haplogranitic liquids and glasses at 200 MPa from hydration–diffusion experiments;Acosta-Vigil;Contributions to Mineralogy and Petrology,2005
4. Dissolution of quartz, albite, and orthoclase in H2O-saturated haplogranitic melts at 800°C and 200 MPa: diffusive transport properties of granitic melts at crustal anatectic conditions;Acosta-Vigil;Journal of Petrology,2006
5. 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;Contributions to Mineralogy and Petrology,2006
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