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Long-term dispersion of river gravel in a canyon in the Atacama Desert, Central Andes, deduced from their (10)Be concentrations
Intense storms or earthquakes in mountains can supply large amounts of gravel to rivers. Gravel clasts then travel at different rates, with periods of storage and periods of displacement leading to their downstream dispersion over millennia. The rate of this dispersion controls the long-term downcut...
| Autores principales: | , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2019
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6882893/ https://www.ncbi.nlm.nih.gov/pubmed/31780673 http://dx.doi.org/10.1038/s41598-019-53806-x |