Some Phase Equilibrium Constraints on the Origin of Proterozoic (Massif) Anorthosites and Related Rocks

1999/02/01 by J. Longhi, Jacqueline Vander Auwera, J. V. Auwera +4 · 3 citations
Earth and Planetary Sciences · #Geological and Geochemical Analysis #High-pressure geophysics and materials #earthquake and tectonic studies

paper · doi:10.1093/petroj/40.2.339

Abstract

peer reviewed

Cited by

• Polybaric Fractional Crystallization of High-alumina Basalt Parental Magmas in the Egersund–Ogna Massif-type Anorthosite (Rogaland, SW Norway) Constrained by Plagioclase and High-alumina Orthopyroxene Megacrysts
• Phase Equilibria of the Lyngdal Granodiorite (Norway): Implications for the Origin of Metaluminous Ferroan Granitoids
• Thermodynamic constraints on the petrogenesis of massif-type anorthosites and their parental magmas

Related

• Petrogenesis of a Mid-Proterozoic Anorthosite-Mangerite-Charnockite-Granite (AMCG) Complex: Isotopic and Chemical Evidence from the Nain Plutonic Suite
• Late-Orogenic, Post-Orogenic, and Anorogenic Granites: Distinction by Major-Element and Trace-Element Chemistry and Possible Origins
• Thermodynamic constraints on the petrogenesis of massif-type anorthosites and their parental magmas
• Origin of Anorthosite and Magnetitite Layers in the Bushveld Complex, Constrained by Major Element Compositions of Plagioclase
• Multivariable phase diagrams; an algorithm based on generalized thermodynamics