Fluvial response to horizontal shortening and glaciations: A study in the Southern Alps of New Zealand

Fluvial response to horizontal shortening and glaciations: A study in the Southern Alps of New Zealand

Source :

• Journal of Geophysical Research: Earth Surface [ 0148-0227 ] ; 2006-03.

English descriptors

• KwdEn :
  • Active mountain belts, Advected, Advection, Advection term, Alpine, Alpine fault, Alps, Asymmetry, Base level, Batt, Beaumont, Beavan, Bedrock, Bedrock incision, Braun, Cascade, Central part, Compressional orogens, Continental collision, Convergence, Convergence velocity, Craw, Critical slope, Crustal, Crustal deformation, Different values, Digital elevation model, Drainage area, Drainage basins, Eastern side, Equilibrium position, Erosion, Erosion rate, Erosional, Fluvial, Fluvial conditions, Fluvial efficiency, Fluvial erosion, Fluvial incision, Fluvial processes, Fluvial response, Geol, Geomorphic, Geomorphology, Geophys, Glacial, Glacial debris, Glacial erosion, Glacial periods, Glaciated, Glaciation, Grid, Hillslope, Hillslope diffusion, Hillslope erosion, Hillslope processes, Horizontal advection, Hovius, Incision, Koons, Landform, Landform evolution, Landscape evolution, Landscape evolution model, Landsliding, Large number, Last glaciation, Main drainage, Maximum slope, Misfit, Misfit function, Misfit value, Mountain belt, Mountain range, Mountain ranges, Numerical experiments, Numerical models, Oblique, Orogen, Orogens, Orographic, Orographic precipitation, Parameter space, Personal communication, Precipitation, Proside, Relief production, Retroside, River profile, River tributaries, Rock uplift, Run1, Run2, Sambridge, Satellite image, Seismic, Seismic strain rate, Southern alps, Southern alps figure, Steady state, Steady state conditions, Surface topography, Tectonic, Tectonic advection, Tectonic model, Tectonic uplift, Tectonics, Tectonomorphic model, Thermochronological data, Time step, Topographic, Topographic balance, Topography, Tributary, Uplift, Uplift rate, Valley floor, Various processes, Velocity field, Western flank, Western side, Whataroa, Whataroa river, Whitehouse, Willett, Zealand.
• Teeft :
  • Active mountain belts, Advected, Advection, Advection term, Alpine, Alpine fault, Alps, Asymmetry, Base level, Batt, Beaumont, Beavan, Bedrock, Bedrock incision, Braun, Cascade, Central part, Compressional orogens, Continental collision, Convergence, Convergence velocity, Craw, Critical slope, Crustal, Crustal deformation, Different values, Digital elevation model, Drainage area, Drainage basins, Eastern side, Equilibrium position, Erosion, Erosion rate, Erosional, Fluvial, Fluvial conditions, Fluvial efficiency, Fluvial erosion, Fluvial incision, Fluvial processes, Fluvial response, Geol, Geomorphic, Geomorphology, Geophys, Glacial, Glacial debris, Glacial erosion, Glacial periods, Glaciated, Glaciation, Grid, Hillslope, Hillslope diffusion, Hillslope erosion, Hillslope processes, Horizontal advection, Hovius, Incision, Koons, Landform, Landform evolution, Landscape evolution, Landscape evolution model, Landsliding, Large number, Last glaciation, Main drainage, Maximum slope, Misfit, Misfit function, Misfit value, Mountain belt, Mountain range, Mountain ranges, Numerical experiments, Numerical models, Oblique, Orogen, Orogens, Orographic, Orographic precipitation, Parameter space, Personal communication, Precipitation, Proside, Relief production, Retroside, River profile, River tributaries, Rock uplift, Run1, Run2, Sambridge, Satellite image, Seismic, Seismic strain rate, Southern alps, Southern alps figure, Steady state, Steady state conditions, Surface topography, Tectonic, Tectonic advection, Tectonic model, Tectonic uplift, Tectonics, Tectonomorphic model, Thermochronological data, Time step, Topographic, Topographic balance, Topography, Tributary, Uplift, Uplift rate, Valley floor, Various processes, Velocity field, Western flank, Western side, Whataroa, Whataroa river, Whitehouse, Willett, Zealand.

Abstract

• https://api.istex.fr/document/C34D1896CF97848336E7A04DA33F235D5B7E688F/fulltext/pdf

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