Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
1042743 | Quaternary International | 2012 | 9 Pages |
Abstract
Alluvial deposits within the Sabaloka Gorge and the Sixth Cataract, the Nile River, Sudan, represent a set of deposits with a high lithological variability. This is due to the geomorphology and short-time and intensive flood events resulting in aggradation and erosion of the alluvial zone. Human maintenance of the alluvial zone also plays a role. Therefore, these sediments seem to be ideal for a methodological case study to show how the lithological facies differ depending on the sedimentary dynamics of the river. Non-magnetic proxies together with TOC values depend on magnetic properties characterized by magnetic susceptibility and its frequency dependence.
Related Topics
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Earth and Planetary Sciences
Geology
Authors
L. Lisa, P. Lisy, M. Chadima, P. Äejchan, A. Bajer, V. Cilek, L. Sukova, P. Schnabl,