Mapping turbidity layers using seismic oceanography methods
Using a combination of seismic oceanographic and physical oceanographic data acquired across the Faroe-Shetland Channel we present evidence of a turbidity layer that transports suspended sediment along the western boundary of the Channel. We focus on reflections observed on seismic data close to the...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2012-01-01
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| Series: | Ocean Science |
| Online Access: | http://www.ocean-sci.net/8/11/2012/os-8-11-2012.pdf |