Dry and strong quartz during deformation of the lower crust in the presence of melt
Granulite facies migmatitic gneisses from the Seiland Igneous Province (northern Norway) were deformed during deep crustal shearing in the presence of melt, which formed by dehydration melting of biotite. Partial melting and deformation occurred during the intrusion of large gabbroic plutons at the...
Published in: | Journal of Geophysical Research |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Geopgysical Union (AGU)
2011
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Subjects: | |
Online Access: | https://hdl.handle.net/10037/3944 https://doi.org/10.1029/2011JB008371 |