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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Bibliographic Details
Main Author: Wikaputri, Devina Anisa
Other Authors: Felix, Maarten
Format: Master Thesis
Language:English
Published: NTNU 2018
Subjects:
Online Access:http://hdl.handle.net/11250/2504050