The erosional and uplift history of NE Atlantic passive margins: constraints on a passing plume

New apatite fission-track analyses from NW Britain indicate that a maximum of 2.5 km of erosion has occurred there during the Cenozoic, similar to values for SE Greenland and the east Greenland coast north of Scoresby Sund. The erosion may have been facilitated by magmatic underplating during break-...

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Bibliographic Details
Published in:Journal of the Geological Society
Main Authors: Clift, P.D., Carter, Andrew, Hurford, A.J.
Format: Article in Journal/Newspaper
Language:unknown
Published: Geological Society of London 1998
Subjects:
Online Access:https://eprints.bbk.ac.uk/id/eprint/28384/
https://doi.org/10.1144/gsjgs.155.5.0787