Origin and evolution of the Kolbeinsey Ridge and Iceland Plateau, N-Atlantic

Variations in crustal structure along the 700 km long KRISE7 refraction/reflection and gravity profile, straddling 66.5 degrees N across the Iceland Shelf, Iceland Plateau and western Norway Basin confirm that extinct spreading centers coexisted with the now extinct aegir Ridge prior to the initiati...

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Bibliographic Details
Published in:Geochemistry, Geophysics, Geosystems
Main Authors: Brandsdottir, Bryndis, Hooft, Emilie E. E., Mjelde, Rolf, Murai, Yoshio
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union
Subjects:
450
Online Access:http://hdl.handle.net/2115/59782
https://doi.org/10.1002/2014GC005540