Polyphasal foreland-vergent deformation in a deep section of the 1 Ga Sveconorwegian orogen
Metamorphic belts in Precambrian shields expose deep interiors of orogens and are often challenging to interpret in tectonic terms. The Eastern Segment of the 1.1-0.9 Ga Sveconorwegian orogen is a metamorphic belt, which was metamorphosed at high-pressure granulite and upper amphibolite facies at 35-40 km depth and shows highly complex fold patterns. We use detailed structural analysis in combinat