Graphical analysis of P—T—X relations in granulite facies metapelites
BJ Hensen, SL Harley - High-temperature metamorphism and crustal …, 1990 - Springer
BJ Hensen, SL Harley
High-temperature metamorphism and crustal anatexis, 1990•SpringerThe study of the complex mineral reactions in metamorphic rocks is facilitated by graphical
representation in the form of chemographic projections and phase diagrams. In this chapter
we discuss and develop the graphical analysis of phase relations in multicomponent
systems containing Fe-Mg solid solutions. Particular emphasis is placed on the relevance of
divariant and univariant equilibria for the interpretation of mineral reactions in high-grade
metapelites.
representation in the form of chemographic projections and phase diagrams. In this chapter
we discuss and develop the graphical analysis of phase relations in multicomponent
systems containing Fe-Mg solid solutions. Particular emphasis is placed on the relevance of
divariant and univariant equilibria for the interpretation of mineral reactions in high-grade
metapelites.
Abstract
The study of the complex mineral reactions in metamorphic rocks is facilitated by graphical representation in the form of chemographic projections and phase diagrams. In this chapter we discuss and develop the graphical analysis of phase relations in multicomponent systems containing Fe-Mg solid solutions. Particular emphasis is placed on the relevance of divariant and univariant equilibria for the interpretation of mineral reactions in high-grade metapelites.
Springer
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