Earthquakes as Precursors of Ductile Shear Zones in the Dry and Strong Lower Crust

The rheology and the conditions for viscous flow of the dry granulite facies lower crust are still poorly understood. Viscous shearing in the dry and strong lower crust commonly localizes in pseudotachylyte veins, but the deformation mechanisms responsible for the weakening and viscous shear localiz...

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Bibliographic Details
Published in:Geochemistry, Geophysics, Geosystems
Main Authors: Menegon, L., Pennacchioni, G., Malaspina, N., Harris, K., Wood, E.
Format: Article in Journal/Newspaper
Language:English
Published: Blackwell Publishing Ltd 2017
Subjects:
Online Access:http://hdl.handle.net/11577/3258747
https://doi.org/10.1002/2017GC007189
http://onlinelibrary.wiley.com/journal/10.1002/(ISSN)1525-2027