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• W2141125790 abstract "Geochronological data indicate that the Caledonian thrust sheets of NW Scotland were assembled in 18 Ma, yet regional Barrovian metamorphism to amphibolite facies and local melting occurred syn-thrusting. From theoretical studies, it is clear that there is insufficient time to generate the high metamorphic temperatures during the thrusting event. We suggest that a plausible explanation for the heat source is that it resulted from a 20–25 Ma period of crustal heating in a back-arc setting between the Grampian and Scandian orogenic events. Most of the orogenic heat therefore came from the pre-existing back-arc rather than the orogenic process itself." @default.
• W2141125790 created "2016-06-24" @default.
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• W2141125790 date "2006-07-01" @default.
• W2141125790 modified "2023-10-17" @default.
• W2141125790 title "A discussion of possible heat sources during nappe stacking: the origin of Barrovian metamorphism within the Caledonian thrust sheets of NW Scotland" @default.
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• W2141125790 doi "https://doi.org/10.1144/0016-764920-168" @default.
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