Garnet could be the ultimate petrochronometer. Not only can you date it directly (with an
accuracy and precision that may surprise some), but it is also a common rock-forming and …

Mineral equilibria calculations in the system K2O–FeO–MgO–Al2O3–SiO2–H2O–TiO2–
Fe2O3 (KFMASHTO) using thermocalc and its internally consistent thermodynamic dataset …

Fe‐rich metapelitic granulites of the Musgrave Block, central Australia, contain several
symplectic and coronal reaction textures that post‐date a peak S2 metamorphic assemblage …

Experimental investigation of the fluid absent melting reaction biotite+ plagioclase+
A12SiOs+ quartz~ garnet+ K-feldspar+ melt at 10 kbar, indicated that melting began …

Garnet-biotite experiments now exist from, FS),, PL), and, GE). Recent garnet Margules
parameters exist from, BA),, GA), and, MU). A comparison of ΔGmix plots for garnet binaries …

At present there are many calibrations of both the garnet–biotite (GB) thermometer and the
garnet–aluminum silicate–plagioclase–quartz (GASP) barometer that may confuse …

Diamondiferous rocks from the Kokchetav Massif, Kazakhstan, represent deeply subducted
continental crust. In order to constrain the age of ultra high pressure (UHP) metamorphism …

Most granitic batholiths contain plutons which are composed of low-variance mineral
assemblages amenable to quantification of the P–conditions that characterise emplacement …

The existing experimental data Ferry and Spear 1978; Perchuk and Lavrent'eva 1983 on
Mg− Fe partitioning between garnet and biotite are disparate. The underlying assumption of …

There are three geothermometers based on reversed experimental data and applicable to
granulites: the two-pyroxene, two-oxide, and garnet-clinopyroxene thermometers. All have …