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A seven-million-year hornblende mineral record from the central Chinese Loess Plateau
Previous studies of the late Cenozoic erosion rate have yielded different views—long-term stable rates or a significant increase at climate transitions—leading to uncertainty concerning the hypothesized global erosion rate controlled by either tectonic uplift or climatic changes. Here, we present a...
| Autores principales: | , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2017
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5443836/ https://www.ncbi.nlm.nih.gov/pubmed/28539632 http://dx.doi.org/10.1038/s41598-017-02400-0 |