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- W2044256323 abstract "Abstract Activity-composition relations in oligoclase near the peristerite gap are investigated in pelites from the Central Menderes Massif. The pressure of metamorphism is estimated independently, from garnet-rutile-ilmenite-kyanite-quartz, as being in the range 4–7 kbar. In the temperature range, 450–600°C approximately, both the Newton-Haselton calibration of the garnet-plagioclase-kyanite-quartz geobarometer and a related simple treatment of garnet-plagioclase-muscovite-biotite give a wide range of apparent pressures, correlated with plagioclase composition and ranging up to 11–12 kbar where the plagioclase is most sodic. This effect is attributed to failure of the activity model for plagioclase used in the Newton-Haselton treatment. It is inferred that, in the present area, γplagAn decreases with increasing XplagAn in the range An15-An25. The data can be interpreted in terms of high γplagAn in the high-albite structure at these temperatures, modified to lower values by ‘e’ordering in the more calcic oligoclases. The ordering appears to be independent of the peristerite gap, and the data do not support the interpretation of the gap as a solvus. Garnet-plagioclase assemblages are unreliable as geobarometers where the plagioclase is more sodic than approximately An20 and T < 700°C, and should instead be used to investigate the γ-X behaviour of the plagioclase where independent geobarometry can be used as a constraint." @default.
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- W2044256323 date "1985-09-01" @default.
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- W2044256323 title "Plagioclase relations in pelites, central Menderes Massif, Turkey. II. Perturbation of garnet-plagioclase geobarometers" @default.
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- W2044256323 doi "https://doi.org/10.1111/j.1525-1314.1985.tb00318.x" @default.
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