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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Auteurs principaux: | , , , |
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Format: | article |
Langue: | EN |
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Nature Portfolio
2021
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Accès en ligne: | https://doaj.org/article/3f67624e8b1d4e0fb3f1bf39c3dde3ff |
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