Amphibole thermodynamics are approximated with the symmetric formalism (regular
solution model for within-site non-ideality and a reciprocal solution model for cross-site …

Although many recent reviews emphasize a uniformity in granulite pressure–temperature (P–
T) conditions and paths, granulites in reality preserve a spectrum of important petrogenetic …

Newly recognized occurrences of ultrahigh-pressure (UHP) minerals including diamonds in
ultrahigh-temperature (UHT) felsic granulites of orogenic belts, in chromitites associated with …

The discovery of diamonds in metamorphic rocks of continental affinities occurred shortly
after the discovery of coesite in similar rocks. These important discoveries led to a revolution …

We present a new compilation of physical properties of minerals relevant to subduction
zones and new phase diagrams for mid‐ocean ridge basalt, lherzolite, depleted lherzolite …

A garnet–hornblende Fe–Mg exchange geothermometer has been calibrated against the
garnet–clinopyroxene geothermometer of Ellis & Green (1979) using data on coexisting …

Two mineralogic geobarometers based on the assemblage garnet-plagioclase-pyroxene-
quartz, common in granulite-grade quartzofeldspathic and basic lithologies, have been …

Experimentally determined pyroxene phase relations at 800°–1200° C are combined with
calculated phase equilibria for the Di‐En and Hd‐Fs joins to produce a graphical two …

This study assesses temperatures of formation of common granulites by combining
experimental constraints on the P–T stability of granulite-facies mineral associations with a …

Calibrations are presented for an independent set of four equilibria between end-members
of garnet, hornblende, plagioclase and quartz. Thermodynamic data from a large internally …