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Large-number detrital zircon U-Pb ages reveal global cooling caused the formation of the Chinese Loess Plateau during Late Miocene

The formation and evolution of the landscape of the Chinese Loess Plateau (CLP) is debated because of uncertainties regarding dust provenance. We present a quantitative estimation of dust source contributions to the CLP, based on more than 37,100 detrital zircon U-Pb ages, combined with mineral asse...

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Detalles Bibliográficos
Autores principales: Zhang, Hanzhi, Lu, Huayu, He, Jing, Xie, Wanting, Wang, Hanlin, Zhang, Hongyan, Breecker, Daniel, Bird, Anna, Stevens, Thomas, Nie, Junsheng, Li, Gaojun
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9555786/
https://www.ncbi.nlm.nih.gov/pubmed/36223463
http://dx.doi.org/10.1126/sciadv.abq2007