Geochemical Changes in the Late Ordovician to Early Silurian Interval in the Northern Margin of the Upper Yangtze Platform, Southern China: Implications for Hydrothermal Influences and Paleocean Redox Circumstances

[Image: see text] A comprehensive chemostratigraphic study, including evaluation of rare earth elements and trace elements, was conducted to explain the paleoenvironments of the northern margin of the Upper Yangtze Platform. Trace elements, like Ba, U, V, Cu, and Zn, tended to be more abundant in th...

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Detalles Bibliográficos
Autores principales: Fu, Xiang, Liu, Xuan, Xiong, Shuzhen, Li, Xu, Wu, Qixuan, Xiao, Bin
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Chemical Society 2023
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10099134/
https://www.ncbi.nlm.nih.gov/pubmed/37065066
http://dx.doi.org/10.1021/acsomega.3c00277

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10099134/
https://www.ncbi.nlm.nih.gov/pubmed/37065066
http://dx.doi.org/10.1021/acsomega.3c00277

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