Article ID Journal Published Year Pages File Type
6445742 Quaternary Science Reviews 2013 16 Pages PDF
Abstract
► High resolution data revealed excellent details of submarine glacial landforms. ► Estimated palaeo-ice stream velocities during LGM were about 350 m/year. ► A rapid early deglaciation in the troughs was followed by a stepwise recession. ► The deglaciation of the banks was characterized by minor halts and readvances. ► The trough widths probably exerted an important control on the deglacial dynamics.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geology
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