Thermal state and evolving geodynamic regimes of the Meso- to Neoarchean North China Craton

Constraining thickness and geothermal gradient of Archean continental crust are crucial to understanding geodynamic regimes of the early Earth. Archean crust-sourced tonalitic–trondhjemitic–granodioritic gneisses are ideal lithologies for reconstructing the thermal state of early continental crust....

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Detalles Bibliográficos
Autores principales: Sun, Guozheng, Liu, Shuwen, Cawood, Peter A., Tang, Ming, van Hunen, Jeroen, Gao, Lei, Hu, Yalu, Hu, Fangyang
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8222299/
https://www.ncbi.nlm.nih.gov/pubmed/34162844
http://dx.doi.org/10.1038/s41467-021-24139-z

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8222299/
https://www.ncbi.nlm.nih.gov/pubmed/34162844
http://dx.doi.org/10.1038/s41467-021-24139-z

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