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• W2316885862 startingPage "235" @default.
• W2316885862 abstract "ABSTRACT The lower Palaeozoic rocks of the Southern Uplands of Scotland have been interpreted as an accretionary prism of slivers of oceanic basalt and associated deep sea sediments situated on the northern margin of the lape tus Ocean. Electron microprobe analyses confirm the presence of albite, prehnite, pumpellyite, chlorite, phengite, calcite, hematite and quartz-bearing metamorphic assemblages in basalts and basic-clast greywackes in the prism. The metamorphism is prehnite-pumpellyite facies and inferred to be related to tectonic burial of the various slices of the prism as they were accreted during the closure of the lape tus Ocean." @default.
• W2316885862 created "2016-06-24" @default.
• W2316885862 creator A5082042636 @default.
• W2316885862 creator A5086214479 @default.
• W2316885862 date "1980-01-01" @default.
• W2316885862 modified "2023-09-25" @default.
• W2316885862 title "Metamorphism in an accretionary prism: prehnite-pumpellyite facies metamorphism of the Southern Uplands of Scotland" @default.
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• W2316885862 doi "https://doi.org/10.1017/s0263593300013602" @default.
• W2316885862 hasPublicationYear "1980" @default.
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