Oscillation of mineral compositions in Core SG-1b, western Qaidam Basin, NE Tibetan Plateau

Uplift of the Tibetan Plateau since the Late Miocene has greatly affected the nature of sediments deposited in the Qaidam Basin. However, due to the scarcity of continuously dated sediment records, we know little about how minerals responded to this uplift. In order to understand this response, we h...

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Detalles Bibliográficos
Autores principales: Fang, Xiaomin, Li, Minghui, Wang, Zhengrong, Wang, Jiuyi, Li, Jiao, Liu, Xiaoming, Zan, Jinbo
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5021985/
https://www.ncbi.nlm.nih.gov/pubmed/27625177
http://dx.doi.org/10.1038/srep32848

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5021985/
https://www.ncbi.nlm.nih.gov/pubmed/27625177
http://dx.doi.org/10.1038/srep32848

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