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f Crustal Transect Across the Lofoten Margin, Northern Norway, Obtained by Use of Ocean Bottom Seismographs
- Publisher: European Association of Geoscientists & Engineers
- Source: Conference Proceedings, 57th EAGE Conference and Exhibition, May 1995, cp-90-00351
- ISBN: 978-90-73781-06-1
Abstract
The continental break-up between Norway and Greenland occurred in late Paleocene / early Eocene, and was associated with an intensive volcanisim along the margin. At a passive continental margin the whole process of crustal evolution is generally retained in the crustal structure from the continent to the ocean.