Table1_Volcanic Structures and Magmatic Evolution of the Vesteris Seamount, Greenland Basin.XLSX

• Main Authors: Katharina A. Unger Moreno (11595160), Janis Thal (11595163), Wolfgang Bach (771394), Christoph Beier (3483125), Karsten M. Haase (5384735)
• Format: Dataset
• Language: unknown
• Published: 2021
• Subjects: Solid Earth Sciences; Climate Science; Atmospheric Sciences not elsewhere classified; Exploration Geochemistry; Inorganic Geochemistry; Isotope Geochemistry; Organic Geochemistry; Geochemistry not elsewhere classified; Igneous and Metamorphic Petrology; Ore Deposit Petrology; Palaeontology (incl. Palynology); Structural Geology; Tectonics; Volcanology; Geology not elsewhere classified; Seismology and Seismic Exploration; Glaciology; Hydrogeology; Natural Hazards; Quaternary Environments; Earth Sciences not elsewhere classified; Evolutionary Impacts of Climate Change; oceanic intraplate volcanism; liquid line of descent; volcanic flanks; effusive and explosive volcanism; submarine volcano morphology; Greenland; Greenland Basin; Cones The; Cones, The; Vesteris Seamount
• Online Access: https://doi.org/10.3389/feart.2021.711910.s003

The formation of isolated seamounts distant from active plate boundaries and mantle plumes remains unsolved. The solitary intraplate volcano Vesteris Seamount is located in the Central Greenland Basin and rises ∼3,000 m above the seafloor with a total eruptive volume of ∼800 km 3 . Here, we present...