Seismic architecture and sedimentology of a major grounding zone system deposited by the Bjørnøyrenna Ice Stream during Late Weichselian deglaciation |
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| Authors: | Denise Christina Rüther Rune Mattingsdal Karin Andreassen Matthias Forwick Katrine Husum |
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| Institution: | 1. Department of Earth Sciences, University of Bergen, Norway;2. Uni Research, Bergen, Norway;3. Bjerknes Centre for Climate Research, Bergen, Norway;1. School of Geography, Archaeology and Palaeoecology, Queen''s University Belfast, Belfast BT7 1NN, UK;2. School of Geography, Queen Mary University of London, Mile End Road, London E1 4NS, UK;3. Department of Geology, The University Centre in Svalbard (UNIS), Longyearbyen N-9171, Norway;1. Physics of Geological Processes (PGP), University of Oslo, P.O. Box 1048, Blindern, 0316 Oslo, Norway;2. Geological Survey of Norway (NGU), P.O. Box 6315, Sluppen, 7491 Trondheim, Norway;3. Centre for Arctic Gas Hydrate, Environment and Climate (CAGE), University of Trømso, 9019 Tromsø, Norway |
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| Abstract: | A 280 km wide sediment wedge in outer Bjørnøyrenna (Bear Island Trough), south-western Barents Sea, has been investigated using 2D and 3D seismic data, sediment gravity cores, as well as regional swath and large scale bathymetry data. The bathymetry data indicate a division into an up to 35 m high frontal wedge with large depressions, and an upstream part characterized by mega scale glacial lineations (MSGL). From seismic sections increasing erosion is demonstrated for the upstream part, coinciding with the location of MSGL. Whether the latter are depositional features postdating an extensive erosional event or formed by erosion remains inconclusive. Based on the distinct morphology and internal structures, we infer that the system was deposited during a rapid readvance whereby the ice front pushed and bulldozed predominantly soft, diluted proglacial sediments. Analyses in the eastern part of the sediment system reveal the existence of imbricated thrust sheets in the frontal part of the wedge. This is suggested to imply upstream erosion of sedimentary rock and incorporation of thrusted blocks into the moraine, forming a composite ridge locally. We argue that observed large scale depressions are dead-ice features in the marine environment. It is envisioned that intense englacial thrusting may have developed into a decollement as the cold glacier snout got overrun by ice masses from the interior, thereby enabling the inclusion of slabs of ice in the push moraine mass. Radiocarbon dates indicate that the sediment wedge was deposited around 17,090 cal yrs BP (14,530 14C yrs BP) and that the ice front probably remained stable until 16,580 cal yrs BP (13,835 14C yrs BP). |
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