Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic
Glacigenic debris-flows represent successive mass-flow deposits that build out a prograding wedge of sediment beyond the grounding zone of an ice sheet (e.g. Laberg & Vorren 1995; King et al. 1998). A prograding sedimentary depocentre extending from the outer shelf to the upper slope has been ob...
| Published in: | Geological Society, London, Memoirs |
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| Main Authors: | , |
| Other Authors: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Geological Society of London
2016
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| Subjects: | |
| Online Access: | http://hdl.handle.net/1893/27900 https://doi.org/10.1144/m46.94 http://dspace.stir.ac.uk/bitstream/1893/27900/1/361.full.pdf |