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

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 edifice, includ...

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Bibliographic Details
Published in:Geochemistry, Geophysics, Geosystems
Main Authors: Beloša, L., Callegaro, S., Meyzen, C. M., Gaina, C., Polteau, S., Bizimis, M., Mazzini, A.
Format: Article in Journal/Newspaper
Language:English
Published: John Wiley and Sons Inc 2024
Subjects:
Online Access:https://hdl.handle.net/11577/3504611
https://doi.org/10.1029/2023GC011196
https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2023GC011196