Uplift-driven sediment redness decrease at ~16.5 Ma in the Yumen Basin along the northeastern Tibetan Plateau

Significant climate shifts in the northeastern Tibetan Plateau have taken place during the Cenozoic, but the reasons behind them remain unclear. In order to unravel the mechanisms driving these climate changes, proxy data with accurate age constraint are needed. Here we present magnetostratigraphy,...

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Detalles Bibliográficos
Autores principales: Wang, Weitao, Zhang, Peizhen, Zheng, Wenjun, Zheng, Dewen, Liu, Caicai, Xu, Hongyan, Zhang, Huiping, Yu, Jingxing, Pang, Jianzhang
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4944177/
https://www.ncbi.nlm.nih.gov/pubmed/27411593
http://dx.doi.org/10.1038/srep29568

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4944177/
https://www.ncbi.nlm.nih.gov/pubmed/27411593
http://dx.doi.org/10.1038/srep29568

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