Devonian–Mississippian magmatism related to extensional collapse in Svalbard: implications for radiating dyke swarms

This work presents the first evidence for extensive Middle Devonian-Mississippian magmatism in Svalbard. These intrusions may be part of the Kola-Dnieper Large Igneous Province and intruded parallel to preexisting, Proterozoic-early Paleozoic orogenic structures. Their strike is inconsistent with a source from a potential mantle plume center in the eastern Barents Sea. Thus, the radiating emplacement pattern of the magmatic intrusions of the Kola-Dnieper Large Igneous Province are not the product of plume-related uplift but of structural inheritance. A similar line of reasoning is successfully applied to intrusions of the Yakutsk-Vilyui and High Arctic large igneous provinces.