Segmentation of the Caledonian orogenic infrastructure and exhumation of the Western Gneiss region during transtensional collapse

The (ultra)high-pressure Western Gneiss Region (WGR) of the Norwegian Caledonides represents an archetypical orogenic infrastructure of a continent-continent collision zone. To test established exhumation models, we synthesize the geochronology and structures of major basement windows and provide ne...

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