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...
Published in: | Geochemistry, Geophysics, Geosystems |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
The Geochemical Society
2024
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Subjects: | |
Online Access: | http://hdl.handle.net/10852/107055 https://doi.org/10.1029/2023GC011196 |