Crustal manifestations of a hot transient pulse at 60°N beneath the Mid-Atlantic Ridge

Since its inception at 62 Ma, mantle convective upwelling beneath Iceland has had a significant influence on Cenozoic vertical motions, magmatism and paleoceanography in the North Atlantic Ocean. Crucially, intersection of the Reykjanes Ridge with the Icelandic Plume provides us with a useful window...

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Bibliographic Details
Published in:Earth and Planetary Science Letters
Main Authors: Parnell-Turner, R.E., White, N.J., Maclennan, J., Henstock, T.J., Murton, B.J., Jones, S.M.
Format: Article in Journal/Newspaper
Language:English
Published: 2013
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/500324/
https://nora.nerc.ac.uk/id/eprint/500324/1/parnell_turner_epsl_2013.pdf
https://doi.org/10.1016/j.epsl.2012.12.030