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- W2094918311 abstract "Effect of pressure on the composition of pyrope-rich garnet coexisting with diopside-rich clinopyroxene and enstatite-rich orthopyroxene in the system MgSiO3-CaSiO3-Al2O3 has been studied in the pressure range 18 to 96 kb and at temperatures between 1390 and 1600°C. It is found that the garnet coexisting with the clinopyroxene and orthopyroxene becomes more pyrope-rich with increase of pressure at constant temperature up to about 70 kb. Pyrope content in the garnet ranges from 81 mol. % at 18 kb to 88% at 71 kb at about 1400°C. Pyrope content in the garnet also increases with decrease of temperature at constant pressure. Alumina content in the clinopyroxene coexisting with the garnet appears to decrease with increase of pressure at constant temperature. From these experimental data, it is suggested that garnet in the garnet peridotite which would constitute most part of the upper mantle becomes more pyrope-rich and clinopyroxene becomes alumina-poor with increase of depth down to at least about 200 km." @default.
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- W2094918311 date "1967-08-01" @default.
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- W2094918311 title "Effect of pressure on garnet-pyroxene equilibrium in the system MgSiO3-CaSiO3-Al2O3" @default.
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- W2094918311 doi "https://doi.org/10.1016/0012-821x(67)90190-2" @default.
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