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...

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Bibliographic Details
Published in:Geophysical Journal International
Main Authors: Smythe, D.K., Chalmers, J.A., Skuce, A.G., Dobinson, A., Mould, A.S.
Format: Article in Journal/Newspaper
Language:unknown
Published: Oxford University Press 1983
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Online Access:http://eprints.gla.ac.uk/213899/