Does Large‐Scale Crustal Flow Shape the Eastern Margin of the Tibetan Plateau? Insights From Episodic Magmatism of Gongga‐Zheduo Granitic Massif

The mechanisms driving crustal deformation and uplift of orogenic plateaus are fundamental to continental tectonics. Large‐scale crustal flow has been hypothesized to occur in eastern Tibet, but it remains controversial due to a lack of geologic evidence. Geochemical and isotopic data from Cenozoic...

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Detalles Bibliográficos
Autores principales: Hu, Fangyang, Wu, Fu‐Yuan, Ducea, Mihai N., Chapman, James B., Yang, Lei
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2022
Materias:
Research Letter
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9287050/
https://www.ncbi.nlm.nih.gov/pubmed/35865913
http://dx.doi.org/10.1029/2022GL098756

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9287050/
https://www.ncbi.nlm.nih.gov/pubmed/35865913
http://dx.doi.org/10.1029/2022GL098756

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