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- W2181653220 abstract "Margarite [CaAl2(Al2SirOto(OH)21 has been found in five pelitic and calcic schist samples in the Solitude Range of the western Rocky Mountains, British Columbia. lt occurs with muscovite, chlorite and biotite in a lepidoblastic texture and is apparently stable in the garnet zone through the kyanite zone. X-ray-diffraction (XRD) analysis of lower-grade slates failed to detect margarite. Geothermobarometry of muscovite-plagioclase-biotite-garnet assemblages suggests temperatures near 580-600oC and pressures near 7 kbar. Margarite + calcite + quartz assemblages persist to temperatures thought to be at or near the stability limit of the assemblage. In the highest-grade occurrences, margarite + plagioclase is present rather than kyanite + clinozoisite, indicating that pressures were probably less than about 7.5 kbar. Fluids that equilibrated with margarite + calcite + plagioclase + clinozoisite were of mixed H2O-CO2 composition." @default.
- W2181653220 created "2016-06-24" @default.
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- W2181653220 date "1991-01-01" @default.
- W2181653220 modified "2023-09-26" @default.
- W2181653220 title "PELITES FROM THE WESTERN ROCKY MOUNTAINS, NORTHWEST OF GOLDEN, BRITISH COLUMBIA" @default.
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- W2181653220 hasPublicationYear "1991" @default.
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