This paper is about the Solund-Hyllestad-Lavik area that affords an excellent opportunity to understand the ultrahigh-pressure Scandian orogeny because it contains a near-complete record of ophiolite emplacement, high-pressure metamorphism and large-scale ...

A granulite-facies Precambrian meta-igneous gneiss complex at Tromy, South Norway, which was previously assumed to represent a fragment of strongly large ion lithophile element (LILE)-depleted lower continental crust, has been reinvestigated using major and ...