Using an internally consistent thermodynamic dataset and updated models of activity---composition relation for solid solu-tions, petrogenetic grids in the system NKFMASH (Na2O---K2O---FeO---MgO---Al2O3---SiO2---H2O) and the subsystems NKMASH and NKFASH have been calculated with the soft-ware THERMOCALC 3.1 in the P---T range 5---36 kbar and 400---810C, involving garnet, chloritoid, biotite, carpholite, talc, chlorite, kyanite/sillimanite, staurolite, phengite, parago
Sapphirine, coexisting with quartz, is an indicator mineral for ultrahigh-temperature metamorphism i...
Internally consistent thermodynamic data for 23 phases in the CaO-Al₂O₃-SiO₂-H₂O system are determin...
A calibration is presented for an activity-composition model for amphiboles in the system Na2O-CaO-F...
Petrogenetic grids in the system NCKFMASH (Na2O-CaO-K2O-FeO-MgO-Al2O3-SiO2-H2O) and the subsystems N...
Pressure–temperature grids in the system Na2O–CaO–K2O–FeO– MgO – Al2O3–SiO2–H2O and its subsystems h...
New activity-composition (a-x) relations for minerals commonly occurring in metapelites are presente...
Petrogenetic grids in the KFMASH and KMnFMASH model systems calculated with the software THERMOCALC ...
Using the updated models of activity-composition relations for solid solutions, P-T pseudosections a...
mproved activity–composition relationships for biotite, garnet and silicate liquid are used to const...
Calorimetric and phase equilibrium data were used to establish an internally consistent thermodynami...
Phase relationships in metapelites were experimentally investigated in the model system CaO-K2O-FeO-...
Thermodynamic modelling of (1) osumilite solid solutions and (2) dehydration melting in pelitic comp...
Cordierite-orthoamphibole gneisses and rocks of similar composition commonly contain low-variance mi...
A set of thermodynamic models is presented that, for the first time, allows partial melting equilibr...
Sapphirine, coexisting with quartz, is an indicator mineral for ultrahigh-temperature metamorphism i...
Sapphirine, coexisting with quartz, is an indicator mineral for ultrahigh-temperature metamorphism i...
Internally consistent thermodynamic data for 23 phases in the CaO-Al₂O₃-SiO₂-H₂O system are determin...
A calibration is presented for an activity-composition model for amphiboles in the system Na2O-CaO-F...
Petrogenetic grids in the system NCKFMASH (Na2O-CaO-K2O-FeO-MgO-Al2O3-SiO2-H2O) and the subsystems N...
Pressure–temperature grids in the system Na2O–CaO–K2O–FeO– MgO – Al2O3–SiO2–H2O and its subsystems h...
New activity-composition (a-x) relations for minerals commonly occurring in metapelites are presente...
Petrogenetic grids in the KFMASH and KMnFMASH model systems calculated with the software THERMOCALC ...
Using the updated models of activity-composition relations for solid solutions, P-T pseudosections a...
mproved activity–composition relationships for biotite, garnet and silicate liquid are used to const...
Calorimetric and phase equilibrium data were used to establish an internally consistent thermodynami...
Phase relationships in metapelites were experimentally investigated in the model system CaO-K2O-FeO-...
Thermodynamic modelling of (1) osumilite solid solutions and (2) dehydration melting in pelitic comp...
Cordierite-orthoamphibole gneisses and rocks of similar composition commonly contain low-variance mi...
A set of thermodynamic models is presented that, for the first time, allows partial melting equilibr...
Sapphirine, coexisting with quartz, is an indicator mineral for ultrahigh-temperature metamorphism i...
Sapphirine, coexisting with quartz, is an indicator mineral for ultrahigh-temperature metamorphism i...
Internally consistent thermodynamic data for 23 phases in the CaO-Al₂O₃-SiO₂-H₂O system are determin...
A calibration is presented for an activity-composition model for amphiboles in the system Na2O-CaO-F...