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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...

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Wedi'i Gadw mewn:
Manylion Llyfryddiaeth
Cyhoeddwyd yn:Sci Rep
Prif Awduron: Madella, Andrea, Delunel, Romain, Akçar, Naki, Schlunegger, Fritz, Christl, Marcus
Fformat: Artigo
Iaith:Inglês
Cyhoeddwyd: Nature Publishing Group UK 2018
Pynciau:
Mynediad Ar-lein: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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