Deep Mantle Component and Continental Crust Remobilization in the Source of Vesteris Seamount, East Greenland Margin

Abstract Vesteris Seamount is a large Quaternary intraplate submarine volcano in the SW Greenland Sea, about 1,000 km NE of Iceland and 300 km NW of the Mohn's spreading ridge, whose mode of formation remains unsolved. We present geochemical data for new samples dredged from the Vesteris edific...

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Bibliographic Details
Published in:Geochemistry, Geophysics, Geosystems
Main Authors: Belosa, Lea, Callegaro, Sara, Meyzen, Christine M, Gaina, Carmen, Polteau, Stephane, Bizimis, Michael, Mazzini, Adriano
Format: Article in Journal/Newspaper
Language:English
Published: The Geochemical Society 2024
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Online Access:http://hdl.handle.net/10852/107055
https://doi.org/10.1029/2023GC011196