A petrologic assessment of internal zonation in granitic pegmatites
Author:
Publisher
Elsevier BV
Subject
Geochemistry and Petrology,Geology
Reference162 articles.
1. Dissolution of corundum and andalusite in H2O-saturated haplogranitic melts at 800°C and 200MPa: constraints on diffusivities and the generation of peraluminous melts;Acosta-Vigil;Journal of Petrology,2002
2. Contrasting interactions of sodium and potassium with H2O in haplogranitic liquids and glasses at 200MPa from hydration–diffusion experiments;Acosta-Vigil;Contributions to Mineralogy and Petrology,2005
3. Dissolution of quartz, albite, and orthoclase in H2O-saturated haplogranitic melt at 800°C and 200MPa: diffusive transport properties of granitic melts at crustal anatectic conditions;Acosta-Vigil;Journal of Petrology,2006
4. Experimental partial melting of a leucogranite at 200MPa 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
5. Chemical diffusion of major and minor components in granitic liquids: implications for the rates of homogenization of crustal melts;Acosta-Vigil;Lithos,2012
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