Garnet pyroxenite from the Shackleton Range, Antarctica: Intrusion of plume-derived picritic melts in the continental lithosphere during Rodinia breakup?

Schmaedicke, E.E.SchmaedickeWill, T.T.WillMezger, KlausKlausMezger0000-0002-2443-85392024-10-242024-10-242015https://boris-portal.unibe.ch/handle/20.500.12422/141524en500 - Science::550 - Earth sciences & geologyGarnet pyroxenite from the Shackleton Range, Antarctica: Intrusion of plume-derived picritic melts in the continental lithosphere during Rodinia breakup?article10.7892/boris.8139810.1016/j.lithos.2015.09.016