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Sættem, Joar; Hamborg, Martin (1987)
Publisher: Co-Action Publishing
Journal: Polar Research
Languages: English
Types: Article
Subjects:
An upper Quaternary seismic unit has been mapped to the east and southeast of Bjern~yrennain the Barents Sea. The unit is dcfined by interpretation of shallow seismic (sparker) data, and occurs as an upper, seismically transparent sequence in the Quaternary succcssion. Discontinuous internal reflections do, however, occasionally occur, especially in the lower part of the unit. The sediments in the unit are interpreted to be of a glaciogenic origin and they most likely consist mainly of tlll.
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    • King. L. H. & Fader. G. B . J . 1986: Wisconsinan glaciation of the Atlantic continental shelf of southeast Canada. Geological Survey of Canada 363, 1-72.
    • King, L. H., Rokoengen. K . & Gunleiksrud. T. 1987: Quaternary seismostratigraphy of Tranabanken and adjacent areas. Continental Shelf Institute Publication no. 114.
    • Solheim, A. & Kristoffersen. Y . 1Y84: The physical environment Western Barents Sea, 1:1,500.000. Sediments above the upper regional unconforrnity: Thickness. seismic stratigraphy and outline of the glacial history. Norsk Polarinstitutt Skr. 1798.
    • Vorren, T. 0..Kristoffersen. Y.& Andreassen. K. 1986: Geology of the inner shelf west of North Cape, Norway. Norsk Geologisk Tidrskrift 66, 99-105.
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