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: | , , |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2012-01-01
|
Series: | Ocean Science |
Online Access: | http://www.ocean-sci.net/8/11/2012/os-8-11-2012.pdf |