Continental crust beneath southeast Iceland

The magmatic activity (0–16 Ma) in Iceland is linked to a deep mantle plume that has been active for the past 62 My. Icelandic and northeast Atlantic basalts contain variable proportions of two enriched components, interpreted as recycled oceanic crust supplied by the plume, and subcontinental litho...

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Veröffentlicht in:	Proceedings of the National Academy of Sciences - PNAS 2015-04, Vol.112 (15), p.E1818-E1827
Hauptverfasser:	Torsvik, Trond H., Amundsen, Hans E. F., Trønnes, Reidar G., Doubrovine, Pavel V., Gaina, Carmen, Kusznir, Nick J., Steinberger, Bernhard, Corfu, Fernando, Ashwal, Lewis D., Griffin, William L., Werner, Stephanie C., Jamtveit, Bjørn
Format:	Artikel
Sprache:	eng
Schlagworte:	Geochemistry Geological time Gravity Greenland Iceland Isotopes lava Lithosphere Magma Physical Sciences PNAS Plus Volcanoes
Online-Zugang:	Volltext
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