Activity coefficients (γ) for grossular in pyrope-grossular garnet have been determined experimentally using the divariant assemblage garnet-anorthite-sillimanite (kyanite)-quartz. Values of γ for garnets with 10-12 mole % grossular have been obtained at 1000 °, 1100 °, 1200 ° and 1300 ° C at pressures between 15 and 21 Kb. The data are consistent with a symmetrical regular solid model for grossular-pyrope solid solutions. The interaction parameter (W) increases linearly with decreasing temperature and is given by W = 7460-4.3 T cals (T in °K). A solvus in the pyrope-grossular solid solution is predicted with a temperature of critical mixing of 629°C±90 ° C. © 1975 Springer-Verlag
Use of simple mixing models of orthopyroxene and garnet solid solutions enables extrapolation of exp...
Static lattice energy calculations, based on empirical pair potentials have been performed for a lar...
An experimental study on melting of pelitic rocks shows that garnet is an important residual phase c...
Garnets on the pyrope-grossular join have been synthesized, their unit-cell edges measured, and the ...
Unit-cell parameters of a series of synthetic garnets with the pyrope, grossular, and four intermedi...
The mixing properties of Fe3Al2Si3O12-Ca3Al2Si3O12 garnet solid solutions have been studied in the t...
We present results of high temperature, high pressure atomistic simulations aimed at determining the...
Experiments were conducted in piston-cylinder apparatus using gels with added H_2O between 900° and...
A series of synthetic pyrope-grossular garnets (Mg3Al2Si3O12-Ca3Al2Si3O12) were investigated by powd...
A series of synthetic pyrope-grossular garnets (Mg3Al2,Si3O12-Ca3Al2Si3O12) were investigated by pow...
This study is composed of two parts. The aim of the first part is to understand the behavior of garn...
Single-phase, well-sintered, translucent polycrystalline garnets with compositions of Py(90)Gr(10) a...
The heat capacities of synthetic pyrope (Mg3Al2Si2O12), grossular (Ca3Al2Si3O12) and a solid solutio...
Applications of the different formulations of garnet-clinopyroxene geothermometers to crustal granul...
The pseudobinary join grossularite-pyrope was investigated at 30 kb nominal pressure at temperature...
Use of simple mixing models of orthopyroxene and garnet solid solutions enables extrapolation of exp...
Static lattice energy calculations, based on empirical pair potentials have been performed for a lar...
An experimental study on melting of pelitic rocks shows that garnet is an important residual phase c...
Garnets on the pyrope-grossular join have been synthesized, their unit-cell edges measured, and the ...
Unit-cell parameters of a series of synthetic garnets with the pyrope, grossular, and four intermedi...
The mixing properties of Fe3Al2Si3O12-Ca3Al2Si3O12 garnet solid solutions have been studied in the t...
We present results of high temperature, high pressure atomistic simulations aimed at determining the...
Experiments were conducted in piston-cylinder apparatus using gels with added H_2O between 900° and...
A series of synthetic pyrope-grossular garnets (Mg3Al2Si3O12-Ca3Al2Si3O12) were investigated by powd...
A series of synthetic pyrope-grossular garnets (Mg3Al2,Si3O12-Ca3Al2Si3O12) were investigated by pow...
This study is composed of two parts. The aim of the first part is to understand the behavior of garn...
Single-phase, well-sintered, translucent polycrystalline garnets with compositions of Py(90)Gr(10) a...
The heat capacities of synthetic pyrope (Mg3Al2Si2O12), grossular (Ca3Al2Si3O12) and a solid solutio...
Applications of the different formulations of garnet-clinopyroxene geothermometers to crustal granul...
The pseudobinary join grossularite-pyrope was investigated at 30 kb nominal pressure at temperature...
Use of simple mixing models of orthopyroxene and garnet solid solutions enables extrapolation of exp...
Static lattice energy calculations, based on empirical pair potentials have been performed for a lar...
An experimental study on melting of pelitic rocks shows that garnet is an important residual phase c...