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(10)Be-inferred paleo-denudation rates imply that the mid-Miocene western central Andes eroded as slowly as today
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 scale. The sa...
| Autores principales: | , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2018
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5797110/ https://www.ncbi.nlm.nih.gov/pubmed/29396427 http://dx.doi.org/10.1038/s41598-018-20681-x |