(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...

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Detalles Bibliográficos
Autores principales: Madella, Andrea, Delunel, Romain, Akçar, Naki, Schlunegger, Fritz, Christl, Marcus
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
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

Internet

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

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