10Be-inferred paleo-denudation rates imply that the mid-Miocene western central Andes eroded as slowly as today
Abstract Terrestrial cosmogenic nuclide concentrations of detrital minerals yield catchment-wide rates at which hillslopes erode. These estimates are commonly used to infer millennial scale denudation patterns and to identify the main controls on mass-balance and landscape evolution at orogenic scal...
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Autores principales: | Andrea Madella, Romain Delunel, Naki Akçar, Fritz Schlunegger, Marcus Christl |
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Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2018
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Materias: | |
Acceso en línea: | https://doaj.org/article/e71e2521142343e69447c96a1ad0e17a |
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