The compositions of multiply saturated partial melts are valuable for the thermodynamic information that the contain, but are difficult to determine experimentally because they exist only over a narrow temperature range at a given pressure. Here we try
Models of formation of basaltic crust at mid-ocean ridges by adiabatic upwelling of fertile mantle ...
The position of the transition from spinel lherzolite to garnet lherzolite in the system CaO-MgO-Al2...
We present the results of melting experiments on a moderately depleted peridotite composition (DMM1)...
The effects of small amounts of H2O (<4wt % in the melt) on the multiply saturated partial melting o...
The effects of small amounts of P2O5 on the partial melting of model spinel lherzolite in the system...
A fully thermodynamic model for mafic melt in CaO–MgO–Al2O3–SiO2 (CMAS) has been calibrated, for cal...
We examine several issues related to peridotite partial melting by performing thermodynamic calculat...
We examine several issues related to peridotite partial melting by performing thermodynamic calculat...
Models of formation of basaltic crust at mid-ocean ridges by adia-batic upwelling of fertile mantle ...
range of temperatures (1380–1505°C) above the carbonated lher- Carbonatites and kimberlites have rec...
We have determined the solidus temperatures and liquid compositions for batch melts of fertile and d...
We have determined the solidus temperatures and liquid compositions for batch melts of fertile and d...
Models of formation of basaltic crust at mid-ocean ridges by adiabatic upwelling of fertile mantle ...
Phase equilibrium experiments on a compositionally modified olivine leucitite from the Tibetan plate...
Models of formation of basaltic crust at mid-ocean ridges by adiabatic upwelling of fertile mantle ...
Models of formation of basaltic crust at mid-ocean ridges by adiabatic upwelling of fertile mantle ...
The position of the transition from spinel lherzolite to garnet lherzolite in the system CaO-MgO-Al2...
We present the results of melting experiments on a moderately depleted peridotite composition (DMM1)...
The effects of small amounts of H2O (<4wt % in the melt) on the multiply saturated partial melting o...
The effects of small amounts of P2O5 on the partial melting of model spinel lherzolite in the system...
A fully thermodynamic model for mafic melt in CaO–MgO–Al2O3–SiO2 (CMAS) has been calibrated, for cal...
We examine several issues related to peridotite partial melting by performing thermodynamic calculat...
We examine several issues related to peridotite partial melting by performing thermodynamic calculat...
Models of formation of basaltic crust at mid-ocean ridges by adia-batic upwelling of fertile mantle ...
range of temperatures (1380–1505°C) above the carbonated lher- Carbonatites and kimberlites have rec...
We have determined the solidus temperatures and liquid compositions for batch melts of fertile and d...
We have determined the solidus temperatures and liquid compositions for batch melts of fertile and d...
Models of formation of basaltic crust at mid-ocean ridges by adiabatic upwelling of fertile mantle ...
Phase equilibrium experiments on a compositionally modified olivine leucitite from the Tibetan plate...
Models of formation of basaltic crust at mid-ocean ridges by adiabatic upwelling of fertile mantle ...
Models of formation of basaltic crust at mid-ocean ridges by adiabatic upwelling of fertile mantle ...
The position of the transition from spinel lherzolite to garnet lherzolite in the system CaO-MgO-Al2...
We present the results of melting experiments on a moderately depleted peridotite composition (DMM1)...
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