Breakup Style and Magmatic Underplating West of the Lofoten Islands, Norway, Based on OBS Data

The breakup of the Northeast Atlantic in the Early Eocene was magma-rich, forming the major part of the North Atlantic Igneous Province (NAIP). This is seen as extrusive and intrusive magmatism in the continental domain, and as a thicker than normal oceanic crust produced the first few million years...

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Bibliographic Details
Main Authors: Breivik, Asbjorn J., Faleide, Jan Inge, Mjelde, Rolf, Murai, Yoshio, Flueh, Ernst R.
Format: Conference Object
Language:unknown
Published: 2014
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/25565/