On the origin and flow behavior of submarine slides on deep-sea fans along the Norwegian–Barents Sea continental margin
作者： A. Solheim , T. Vorren , A. Elverhøi , H. Norem , E. S. Andersen
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摘要: Debris lobes with characteristic lengths, widths, and thickness of 30–200 km, 2–10 km, 10–50 m, respectively, represent the main building blocks deep-sea fans along Norwegian–Barents Sea continental margin. Their formation is closely related to input clay-rich sediments upper slope by glaciers during periods maximum ice advance. It likely that slide release was a consequence an instability arising from high sedimentation rates on slope. The flow behavior debris can be described Bingham model.
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