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In the Seve Nappe Complex on Mt. Grapesvare, Swedish Caledonides, coronitic dolerites and eclogites occur in psammitic and pelitic schists. The transition between them is a 200 m wide zone with small boudins of garnet amphibolite. That zone trends N95°E and does not coincide with any tectonic discontinuity. The intensity of deformation and the lithology of the host rock do not change at the transi
