MARINE GEOLOGY, vol.237, pp.37-53, 2007 (SCI-Expanded)
High-resolution acoustic data indicate that sediment erosion is a significant process in the continental slope of Yesilirmak River Fan, occurring both related to the submarine canyons and in the open continental slope. The sediment processes observed along the slope consist of sliding and debris flows on the canyon walls together with the recent erosional surfaces at the canyon heads wherever the canyons exist, and slides and related scarp features structurally controlled by rotational faults in the central part of the open continental slope.