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...
Published in: | Geochemistry, Geophysics, Geosystems |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Geophysical Union
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Subjects: | |
Online Access: | http://hdl.handle.net/2115/59782 https://doi.org/10.1002/2014GC005540 |