Abstract
The large glacier-fed submarine fan off the western Barents Sea continental shelf, the Bear Island Trough Mouth Fan [Vorren et al., 1989] covers an area of about 240,000 km2. As revealed from both high resolution sparker and 3.5 kHz records, gravity cores and long-range side scan data, the Mid and Late Pleistocene succession is dominated by debris flow deposits, separated by thin interglacial/interstadial hemipelagic sediments [Damuth, 1978; Vorren et al., 1989; Vogt et al., 1993; Laberg and Vorren, 1995, 1996a; Dowdeswell et al., this volume]. A similar stratigraphy characterizes other high-latitude fans [King, this volume; Laberg and Vorren, 1996b].
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© 1997 Chapman & Hall
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Laberg, J.S., Vorren, T.O. (1997). Debris Flow Deposits on a Glacier-fed Submarine fan off the Western Barents Sea Continental Shelf. In: Davies, T.A., et al. Glaciated Continental Margins. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-5820-6_45
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DOI: https://doi.org/10.1007/978-94-011-5820-6_45
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