Evidence for a major sediment input point into the Faroe-Shetland Basin from the Kangerlussuaq region of southern East Greenland
Studies of the sedimentary succession in Kangerlussuaq, southern East Greenland suggest that a prominent sediment input point existed in the region in the Late Cretaceous–Palaeogene, which was controlled by a major northwest–southeast-oriented fault lineament. The presence of this sediment transfer...
Published in: | Geological Society, London, Petroleum Geology Conference series |
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Main Authors: | , |
Other Authors: | , |
Format: | Book Part |
Language: | unknown |
Published: |
Geological Society
2005
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Subjects: | |
Online Access: | http://eprints.esc.cam.ac.uk/1541/ https://doi.org/10.1144/0060913 |