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...
Published in: | Geochemistry, Geophysics, Geosystems |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Blackwell Publishing Ltd
2017
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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 |