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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...
Autores principales: | , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
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Nature Publishing Group UK
2022
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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 |