@ARTICLE{Kowalewski_Włodzimierz_Seismoacoustic_1990, author={Kowalewski, Włodzimierz and Rudowski, Stanisław and Zalewski, S. Maciej}, volume={vol. 11}, number={No 3-4}, journal={Polish Polar Research}, pages={287-300}, howpublished={online}, year={1990}, publisher={Polish Academy of Sciences}, publisher={Committee on Polar Research}, abstract={On the ground of results obtained by the seismoacoustic profiling carried out in 1985 and primary examination of core samples the following main seismoacoustic units are distinguished and characterized: unit A — bedrock, unit B — till and/or compacted glaciomarine deposit, unit C — glaciomarine ice-front deposit, unit D — glaciomarine mud. These results enabled to present the distribution of seismoacoustic units along the fiord and its extension on the shelf, as well as to determine a relation of bottom structures to Late Vistulian(?) deglaciation and the action of Holocene tributary glaciers, probably during the Little Ice Age. The position of marginal structures corresponding to local retreat stages of the glacier front is also presented.}, type={Article}, title={Seismoacoustic studies within Wijdefjorden, Spitsbergen}, URL={http://www.czasopisma.pan.pl/Content/111193/PDF-MASTER/1990-3-4_287-300.pdf}, keywords={Arctic, Spitsbergen, bottom sediments, geophysics}, }