Crystallization conditions of peraluminous charnockites: constraints from mineral thermometry and thermodynamic modelling
Abstract
Most igneous charnockites are interpreted to have crystallized at hot and dry conditions, i.e. at >800 °C and <3 wt.% H2O and with an important CO2 component in the system. These charnockites are metaluminous to weakly peraluminous and their formation involves a significant mantle-derived component. This study, in contrast, investigates the crystallization conditions of strongly peraluminous, metasediment-sourced charnockites from the Qinzhou...
Paper Details
Title
Crystallization conditions of peraluminous charnockites: constraints from mineral thermometry and thermodynamic modelling
Published Date
Apr 3, 2017
Volume
172
Issue
5
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