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- W2075788454 abstract "Summary Paragonite has been found in two chloritoid-chlorite-mica schists from the Dalradian, north of Stonehaven. The principal bulk-chemical constraints on the occurrence of this mineral within the chloritoid zone appear to be the ratios of soda to potash and the Al 2 O 3 contents of the rock. The composition of paragonite coexisting with muscovite indicates a crystallization temperature of 550 °C for rocks some way above the chloritoid isograd. Although this result is supported by other mineral equilibria, the muscovite compositions suggest a temperature of 690 °C which is too high because the mineral assemblage chloritoid-paragonite is unstable above about 600 °C By combining data on the breakdown of the chloritoid-paragonite assemblage with a mineral equilibrium for the assemblage garnet-plagioclase-muscovite-biotite, it has been deduced that rocks close to the staurolite isograd crystallized at about 7·5 kb and 600 °C." @default.
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- W2075788454 date "1977-06-01" @default.
- W2075788454 modified "2023-09-26" @default.
- W2075788454 title "The occurrence of paragonite in chloritoid schists from Stonehaven, Scotland" @default.
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- W2075788454 doi "https://doi.org/10.1180/minmag.1977.041.318.08" @default.
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