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...

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Bibliographic Details
Published in:Journal of Geophysical Research
Main Authors: Menegon, Luca, Nasipuri, Pritam, Stunitz, Holger, Behrens, Harald, Ravna, Erling J Krogh
Format: Article in Journal/Newspaper
Language:English
Published: American Geopgysical Union (AGU) 2011
Subjects:
Online Access:https://hdl.handle.net/10037/3944
https://doi.org/10.1029/2011JB008371