The origin of massive diamicton facies by iceberg rafting and scouring, Scoresby Sund, East Greenland
ABSTRACT Almost 90% of 39 m of core material recovered from Scoresby Sund and the adjacent East Greenland shelf is massive diamicton, interpreted to be formed predominantly by the release of iceberg rafted debris and reworking by iceberg scouring. There is also likely to be a contribution from suspe...
Published in: | Sedimentology |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
1994
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Subjects: | |
Online Access: | http://dx.doi.org/10.1111/j.1365-3091.1994.tb01390.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-3091.1994.tb01390.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-3091.1994.tb01390.x |