Evaluation of grain boundaries as percolation pathways in quartz-rich continental crust using Atomic Force Microscopy

Hydrous fluids play a vital role in the chemical and rheological evolution of ductile, quartz-bearing continental crust, where fluid percolation pathways are controlled by grain boundary domains. In this study, widths of grain boundary domains in seven quartzite samples metamorphosed under varying c...

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Detalles Bibliográficos
Autores principales: Dobe, Ritabrata, Das, Anuja, Mukherjee, Rabibrata, Gupta, Saibal
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/PMC8111022/
https://www.ncbi.nlm.nih.gov/pubmed/33972600
http://dx.doi.org/10.1038/s41598-021-89250-z

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8111022/
https://www.ncbi.nlm.nih.gov/pubmed/33972600
http://dx.doi.org/10.1038/s41598-021-89250-z

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