Abstract: Subaquatic mass movements are common in marine and lacustrine environments, but due to their barely pre- dictable nature, direct observations of these processes are limited so that knowledge is only indirectly obtained by investigating the resulting mass-transport deposits (MTDs). Most research focuses on the most common fron- tally emergent slides, fast-moving events able to generate turbidity currents and tsunamis. Geohazards of fron- tally confined slides and mechanisms behind their typical fold-and-thrust deformation structures are however ...
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