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...
Main Authors: | , , , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2014
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Subjects: | |
Online Access: | https://oceanrep.geomar.de/id/eprint/25565/ |