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...

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Bibliographic Details
Published in:Sedimentology
Main Authors: DOWDESWELL, JULIAN A., WHITTINGTON, ROBERT J., MARIENFELD, PETER
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1994
Subjects:
Online Access:http://dx.doi.org/10.1111/j.1365-3091.1994.tb01390.x
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