A phlogopite-bearing lithospheric mantle source for Europe's largest REE-HFSE belt: Gardar Rift, SW Greenland

Author:

Beard Charles D.ORCID,Finch Adrian A.ORCID,Borst Anouk M.,Goodenough Kathryn M.,Hutchison WilliamORCID,Millar Ian L.,Andersen Tom,Williams Helen M.,Weller Owen M.

Publisher

Elsevier BV

Reference71 articles.

1. Formation of rare Earth deposits in carbonatites;Anenburg;Elements,2021

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3. The complex tectonic evolution of the craton-adjacent northern margin of the Palaeoproterozoic Ketilidian Orogen, southeastern Greenland: evidence from the geochemistry of mafic to intermediate and granitic intrusions;Bagas;Lithos,2020

4. Petrological and geochemical characteristics of Mesoproterozoic dyke swarms in the Gardar Province, South Greenland: evidence for a major sub-continental lithospheric mantle component in the generation of the magmas;Bartels;Mineral. Mag.,2015

5. Mesoproterozoic dykes in the Timmiarmiit area, Southeast Greenland: evidence for a continuous Gardar dyke swarm across Greenland's North Atlantic Craton;Bartels;GFF,2016

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