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

Abstract 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...

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Autores principales: Ritabrata Dobe, Anuja Das, Rabibrata Mukherjee, Saibal Gupta
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/3f67624e8b1d4e0fb3f1bf39c3dde3ff
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