Magmatic evolution and architecture of an oceanic intraplate volcano: Vesteris Seamount, Atlantic Ocean
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DOI: 10.3389/feart.2024.1501694
Abstract: Vesteris is a large (33 × 27 km) and young (summit age: 0.65–0.010 Ma) intraplate seamount in the Greenland Sea, formed from ocean island basalt (OIB) magmatism. The volcano is composed of alkali basalt, basanite/tephrite, phonotephrite,… read more here.
Keywords: architecture; mafic recharge; intraplate; volcano ... See more keywords