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- > HEIMSATH, A., (Editeur scientifique) (supprimer)
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Par Collection Par Auteur- HEIMSATH, A., (Editeur scientifique) (3)
- PERG, L.A. (1)
- ROBERT, X. (1)
- STONE, J.O.H. (1)
- BALCO, G. (1)
- BRAUN, J. (1)
- PARKER, G. (1)
- 2005 (3)
- Analyse isotopique ; Badland ; Dynamique de versant ; Erosion des sols ; Modèle ; Technique de recherche ; Versant ; Vitesse d'érosion (1)
- Analyse isotopique ; Etats-Unis ; Pléistocène ; Quaternaire ; Stratigraphie ; Tectonique ; Utah ; Variation climatique ; Vitesse d'érosion (1)
- Badland ; Erosion rate ; Isotope analysis ; Model ; Research technique ; Slope ; Slope dynamics ; Soil erosion (1)
- China ; Erosion ; Erosion rate ; Geochronology ; Heat flow ; Isostasy ; Mountain ; Numerical model ; Tectonics ; Topography (1)
- Chine ; Dabie Shan ; Erosion ; Flux thermique ; Géochronologie ; Isostasie ; Modèle numérique ; Montagne ; Tectonique ; Topographie ; Vitesse d'érosion (1)
- Climatic variation ; Erosion rate ; Isotope analysis ; Pleistocene ; Quaternary ; Stratigraphy ; Tectonics ; United States of America ; Utah (1)
- Constraints on the rate of post-orogenic erosional decay from low-temperature thermochronological data : application to the Dabie Shan, China (1)
- Measuring middle Pleistocene erosion rates with cosmic-ray-produced nuclides in buried alluvial sediment, Fisher Valley, southeastern Utah (1)
- Probabilistic formulation of conservation of cosmogenic nuclides : effect of surface elevation fluctuations on approach to steady state (1)
- The AA. consider the importance of the lithosphere flexural strength on the isostatic response of the system to erosion. Using a numerical method to solve the heat transport equation in 3 dimensions, the AA. show how a synthetic age distribution can
- be computed and how it is affected by their assumption about the isostatic response of the lithosphere to surface unloading. The AA. then investigate whether the age distribution is sensitive to the assumed erosional response time. Finally they use
- The AA. describe how measurements of the cosmic-ray-produced radionuclides Be 10 and Al 26 in alluvial sediment can be used to develop a continuous record of erosion rate changes through time. The AA. illustrate the method, and evaluate its
- uncertainty and thus usefulness in realistic situations, with an example from a middle Pleistocene alluvial section in Fisher Valley, Utah. Finally, they suggest how it might best be employed in future to answer questions about the relationship of climate
- . The AA. outline how the model can be generalized to basins dominated by deep-seated landslides and to transport-limited, soil-mantled hillslopes.