Research paperGrowth and burial of a submarine canyon off Motunau, North Canterbury, New Zealand
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Cited by (15)
Morphology of submarine canyons along the continental margin of the Potiguar Basin, NE Brazil
2015, Marine and Petroleum GeologyCitation Excerpt :This stage is represented by shelf-incised submarine canyons. The canyon heads act as catchment areas for shelf and river sediments (Green, 2009; Herzer and Lewis, 1979; Mullenbach et al., 2004) that bypass the slope through the canyon valleys and are deposited on the basin floor. Downward sediment flows due to gravity can contribute significantly to canyon excavation and enlargement by a process of axial incision (Baztan et al., 2005; Pratson and Coakley, 1996).
Morphology and controls on the evolution of a mixed carbonate-siliciclastic submarine canyon system, Great Barrier Reef margin, north-eastern Australia
2011, Marine GeologyCitation Excerpt :This stage is represented by shelf-incised submarine canyons (Type 1). The canyon heads act as catchment areas for shelf and river sediments (Herzer and Lewis, 1979; Mullenbach et al., 2004; Green, 2009) that bypass the slope through the canyon valleys and are deposited on the basin floor. Submarine canyons become more active due to the increased sediment supply provided from different areas on the shelf.
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