Early opening history of the North Atlantic - I. Structure and origin of the Faeroe-Shetland Escarpment.
Marine geophysical surveys show that the Escarpment is the buried feather-edge of a thick pile of flood basalts of early Eocene age, overlying a thinner, more widespread layer of basalts of late Palaeocene age. The Escarpment does not, therefore, define the continent—ocean boundary in the southern N...
Published in: | Geophysical Journal International |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Oxford University Press
1983
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Subjects: | |
Online Access: | http://eprints.gla.ac.uk/213899/ |