Abstract
The Scoresby Sund, located in the central part of East Greenland (Fig. 1), is one of the largest fjord systems of the world. Several narrow deep fjords open into the wider shallower parts supplying a large number of icebergs. The sedimentary distribution and structures in this fjord system are strongly influenced by former ice shelf/sheet configurations and recent iceberg movements. Scoresby Sund is characterised by two distinct seismic sequences: a thin Quaternary layer on top of probably Mesozoic sedimentary rocks [Uenzelmann-Neben, 1993].
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Dowdeswell, J.A.; Uenzelmann-Neben, G.; Whittington, R.J.; Marienfeld, P., The Late Quaternary sedimentary record in Scoresby Sund, East Greenland. Boreas, 23, 294: 310, 1994.
Uenzelmann-Neben, G., Scoresby Sund, East Greenland: Structure and distribution of sedimentary rocks. Polarforschung, 62, 1: 9, 1993.
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© 1997 Chapman & Hall
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Uenzelmann-Neben, G. (1997). Structures in Scoresby Sund, East Greenland. In: Davies, T.A., et al. Glaciated Continental Margins. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-5820-6_8
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DOI: https://doi.org/10.1007/978-94-011-5820-6_8
Publisher Name: Springer, Dordrecht
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