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Submarine landslides geohazard along the southern margin of the colombian caribbean : relation to ground conditions and effect on shaping seafloor geomorphology
(Universidad EAFITDoctorado en Ciencias de la TierraEscuela de Ciencias Aplicadas e Ingeniería. Departamento de Ciencias de la TierraMedellín, 2023)
Submarine landslides are a mixture of rock, soil, and fluids moving downslope due to a slope's initial event of mechanical failure. These phenomena play a significant role in the evolution of continental margins. On the ...
Substrate entrainment, depositional relief, and sediment capture: Impact of a submarine landslide on flow process and sediment supply
(Frontiers Media, 2021-11)
Submarine landslides can generate complicated patterns of seafloor relief that influence subsequent flow behaviour and sediment dispersal patterns. In subsurface studies, the term mass transport deposits (MTDs) is commonly ...
Pore‐scale simulation of immersed granular collapse : implications to submarine landslides
(American Geophysical Union; Wiley, 2020)
Geomorphology and sedimentary features of the Simpson Submarine Canyon, 44°S, southern Chilean margin
(Pontificia Universidad Católica de Valparaíso, 2022)
The Carboniferous MTD Complex at La Peña Canyon, Paganzo Basin (San Juan, Argentina)
(Wiley, 2019)
The La Peña Canyon section (San Juan Province, western Argentina) provides outstanding examples of different varieties of mass‐transport deposits (MTDs) and related sediments, showing a wide range of lithologies (from mud ...
Block Generation, Deformation, and Interaction of Mass‐Transport Deposits With the Seafloor: An Outcrop‐Based Study of the Carboniferous Paganzo Basin (Cerro Bola, NW Argentina)
(Wiley, 2019)
Mass‐transport processes are notorious for their ability to carry large blocks or megaclasts, to deform sediments, and to interact with the seafloor through deformation and/or erosion of the substrate. These processes, ...
Active faulting, submarine surface rupture, and seismic migration along the liquine-ofqui fault system, Patagonian Andes
(Amer Geophysical Union, 2020)
The intra-arc Liquine-Ofqui Fault System (LOFS) is an active transpressive fault zone located in the Patagonian Andes of Chile. In 2007, a seismic sequence occurred in the Aysen Fjord region of Chilean Patagonia along the ...