@ARTICLE{Kowalewski_Włodzimierz_Seismostratigraphy_1987, author={Kowalewski, Włodzimierz and Rudowski, Stanisław and Zalewski, S. Maciej and Żakowicz, Krystyna}, volume={vol. 8}, number={No 1}, journal={Polish Polar Research}, pages={3-23}, howpublished={online}, year={1987}, publisher={Polish Academy of Sciences}, publisher={Committee on Polar Research}, abstract={The paper presents results of investigations of bottom sediments in Hornsund, Wijdefjorden and Isfjorden as well as of the shelf around the Bjornoya. carried out in 1982—1985 by a continuous seismic profiling. Geophysic structures and bottom sediments on the bedrock to a depth of 170 ms have been recognized, particularly in the Hornsund region. The following seismoacoustic units have been distinguished: unit A — bedrock, unit В — till and/or compacted glaciogenic deposit, unit С — glaciomarine ice-front deposit, unit D — glaciomarine mud. These results allowed to present a model of glaciomarine sedimentation in a fiord, fed by warm tidewater glaciers.}, type={Article}, title={Seismostratigraphy of bottom sea sediments in some areas of the Spitsbergen Archipelago}, URL={http://www.czasopisma.pan.pl/Content/111358/PDF/1987_1_003-023.pdf}, keywords={Arctic, Spitsbergen, geophysics, seismoacoustic, bottom sediments}, }