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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...
Guardat en:
| Publicat a: | Sci Rep |
|---|---|
| Autors principals: | , , , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Nature Publishing Group UK
2018
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5797110/ https://ncbi.nlm.nih.gov/pubmed/29396427 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-018-20681-x |
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