Abstract
The Friningen Peridotite Lens, found in N. Jämtland, Central Sweden is a tectonically emplaced garnet peridotite lens located in the Seve Nappe Complex (SNC) of the Scandinavian Caledonides. The peridotite records older protolith mineral assemblages than the host gneisses and is crosscut by a basic garnet pyroxenite dike. Metamorphism in
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