Metamorphic processes and seismicity: The Bergen Arcs as a natural laboratory

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Metamorphic processes and seismicity: The Bergen Arcs as a natural laboratory

In the Bergen Arcs rocks that formed the root zone of the Caledonian mountain chain formed by the collision of Laurentia and Baltica at ~400 Ma are exposed. They display a well-exposed, highgrade metamorphic terrane where Sveconorwegian granulites and Caledonian eclogite and amphibolite parageneses...

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Bibliographic Details
Main Authors:	Putnis, Andrew, Jamtveit, B., Austrheim, H.
Format:	Journal Article
Published:	Oxford University Press 2017
Online Access:	http://hdl.handle.net/20.500.11937/67553

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