@article{vagnes_late_1993,
	title = {Late {Cenozoic} uplift and volcanism on {Spitsbergen}: {Caused} by mantle convection?},
	volume = {21},
	issn = {0091-7613},
	shorttitle = {Late {Cenozoic} uplift and volcanism on {Spitsbergen}},
	url = {https://doi.org/10.1130/0091-7613(1993)021<0251:LCUAVO>2.3.CO;2},
	doi = {10.1130/0091-7613(1993)021<0251:LCUAVO>2.3.CO;2},
	abstract = {Regional tectonic uplift, heat-flow measurements, and P-T estimates on upper-mantle xenoliths associated with Neogene volcanic rocks indicate a strongly thinned (∼50 km thick) lithosphere beneath Svalbard, 650 km north of Scandinavia. Data on Neogene volcanic rocks and xenoliths indicate an ∼50 °C temperature anomaly in the underlying asthenosphere, together with volatile-rich conditions in the upper mantle. The Svalbard uplift is one of several Cenozoic epeirogenic uplifts along the margins of the North Atlantic. Boundary processes occurring where hot-spot-influenced asthenosphere abuts cold, deep continental lithosphere seem to be likely explanations for the uplifts.},
	number = {3},
	urldate = {2022-09-28},
	journal = {Geology},
	author = {Vågnes, Erling and Amundsen, Hans Erik Foss},
	month = mar,
	year = {1993},
	pages = {251--254},
}

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