Abstract
The first evidence of UHP metamorphism in the Seve Nappe Complex of northern Jämtland, central Swedish
Caledonides, was discovered in 2010 (Majka & Janák 2011). The UHP parageneses occur within a kyanite-bearing
eclogite, forming part of a metabasic dyke that truncates an orogenic garnet peridotite body. This kyanite-eclogite
provides key information about the
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