Abstract
Orogenic peridotites can be found at or close by the tectonic interfaces between various nappes that make up the Seve-Köli nappe complex (SKNC) in Northern Jämtland, Sweden. These orogenic peridotites have already been found to have different origins, from suboceanic lithospheric mantle (SOLM) to sub-continental lithospheric mantle (SCLM). Several models
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