Widespread overspill from a saline density-current channel and its interaction with topography on the south-west Black Sea shelf

Author:

Hiscott Richard N.1,Aksu Ali E.1,Flood Roger D.2,Kostylev Vladimir3,Yaşar Doğan4

Affiliation:

1. Earth Sciences Department; Memorial University of Newfoundland; St. John's Newfoundland A1B 3X5 Canada

2. Marine Sciences Research Center; Stony Brook University; Stony Brook New York USA

3. Environmental Marine Geology; Geological Survey of Canada - Atlantic; Bedford Institute of Oceanography; Dartmouth Nova Scotia B2Y 4A2 Canada

4. Institute of Marine Sciences and Technology; Dokuz Eylül University; Haydar Aliyev Caddesi No: 10 Inciralı Izmir 35340 Turkey

Publisher

Wiley

Subject

Stratigraphy,Geology

Reference67 articles.

1. Seismic stratigraphy of Late Quaternary deposits from the southwestern Black Sea shelf: evidence for non-catastrophic variations in sea-level during the last ~10,000 years;Aksu;Mar. Geol.,2002

2. Observations on experimental, nonchannelized high-concentration turbidity currents and variations in deposits around obstacles;Alexander;J. Sed. Res.,1994

3. Effects of obstacle heights on controlling turbidity currents with different concentrations and discharges;Asghari Pari;J. Food Agr. Environ.,2010

4. A note on lee wave structures in stratified flow over three-dimensional obstacles;Castro;Tellus,1987

5. Experiments on wave breaking in stratified flow over obstacles;Castro;J. Fluid Mech.,1993

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