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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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Podrobná bibliografie
Vydáno v:Sci Rep
Hlavní autoři: Wang, Weitao, Zhang, Peizhen, Zheng, Wenjun, Zheng, Dewen, Liu, Caicai, Xu, Hongyan, Zhang, Huiping, Yu, Jingxing, Pang, Jianzhang
Médium: Artigo
Jazyk:Inglês
Vydáno: Nature Publishing Group 2016
Témata:
On-line přístup:https://ncbi.nlm.nih.gov/pmc/articles/PMC4944177/
https://ncbi.nlm.nih.gov/pubmed/27411593
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep29568
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