Flow Transformation in Lower and Upper Turbidite Units, NE Helgeland Basin, Offshore Mid-Norway
Sediment transport towards the ocean floor is mainly by sediment gravity flows, either dominated by one flow process such as a slide, slump, debris flow or turbidity current, or more complex flows combining e.g. debris flows and turbidity currents (transitional flows). However, the expected product...
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Format: | Master Thesis |
Language: | English |
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NTNU
2018
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Online Access: | http://hdl.handle.net/11250/2504050 |