Multiple ice age cycles spanning the last three million years have fundamentally transformed the Arctic landscape. The cadence, intensity and pattern of this glacial modification underpin …
A Lasabuda, JS Laberg, SM Knutsen… - Marine and petroleum …, 2018 - Elsevier
The Cenozoic pre-glacial development of the southwestern Barents Sea is discussed, with focus on the early to middle Cenozoic net erosion that was poorly constrained. From 2D and …
F Tsikalas, OA Blaich, JI Faleide… - Geological Society …, 2025 - lyellcollection.org
Abstract The Stappen High–Bjørnøya Tectono-Sedimentary Element (TSE) is located in the western Barents Shelf and is one of the prominent tectonic elements in the area. The …
A Amantov, W Fjeldskaar - Journal of Geodynamics, 2018 - Elsevier
Fennoscandia and Arctic shelves are known to have experienced several periods of Meso- Cenozoic uplift and erosion, but their magnitude and timing are still debated. The aim of our …
KJ Zieba, A Grøver - Marine and Petroleum Geology, 2016 - Elsevier
Previous work indicates that a part of hydrocarbon loss from traps in the Barents Sea is attributed to the Pleistocene (glacially-related) spillage due to isostatically-driven depth …
W Van Der Wal, T IJpelaar - Solid Earth, 2017 - se.copernicus.org
Models for glacial isostatic adjustment (GIA) routinely include the effects of meltwater redistribution and changes in topography and coastlines. Since the sediment transport …
The topographic relief of the Barents Sea was subjected to major changes during the past 1.5 million years mostly due to sediment redistribution driven by glacial activity. This paper …