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-...
Published in: | Journal of the Geological Society |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Geological Society of London
1998
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Subjects: | |
Online Access: | https://eprints.bbk.ac.uk/id/eprint/28384/ https://doi.org/10.1144/gsjgs.155.5.0787 |