Triassic Channel Systems on the northern Loppa High, SW Barents Sea

During the Triassic, the Barents Sea Basin was filled with sediments from the Uralian and Caledonian mountain belts. High sediment yield and large river systems made progradation possible, resulting in an alluvial to deltaic plain stretching from the mountain belts in the south east to Spitsbergen i...

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Bibliographic Details
Main Author: Arntzen, Marit
Format: Master Thesis
Language:English
Published: UiT Norges arktiske universitet 2018
Subjects:
Online Access:https://hdl.handle.net/10037/12905