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...

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Bibliographic Details
Published in:Geological Society, London, Petroleum Geology Conference series
Main Authors: Larsen, M., Whitham, A. G.
Other Authors: Doré, A. G., Vining, B.
Format: Book Part
Language:unknown
Published: Geological Society 2005
Subjects:
Online Access:http://eprints.esc.cam.ac.uk/1541/
https://doi.org/10.1144/0060913