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Increased erosion of high-elevation land during late Cenozoic: evidence from detrital thermochronology off-shore Greenland

Mountain regions at high altitudes show deeply incised glacial valleys that coexist with a high-standing low-relief landscape, whose origin is largely debated. Whether the plateaus contributed to sediment production during the late Cenozoic is a currently debated issue in glacial geomorphology and p...

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Detalles Bibliográficos
Autores principales: Olivetti, Valerio, Cattò, Silvia, Zattin, Massimiliano
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9200846/
https://www.ncbi.nlm.nih.gov/pubmed/35705648
http://dx.doi.org/10.1038/s41598-022-14129-6