High-temperature fracturing and subsequent grain-size-sensitive creep in lower crustal gabbros: Evidence for coseismic loading followed by creep during decaying stress in the lower crust

The mechanism of shear zone formation in lower crustal, relatively “dry” rocks is still poorly understood. We have studied the high-temperature deformation of the Hasvik gabbro (northern Norway) which commences by fracturing. The 10–20 μm wide fractures show little displacement. The fine-grained pla...

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Bibliographic Details
Published in:Journal of Geophysical Research: Solid Earth
Main Authors: Okudaira, Takamoto, Jeřábek, Petr, Stunitz, Holger, Fusseis, Florian
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2015
Subjects:
Online Access:https://hdl.handle.net/10037/24951
https://doi.org/10.1002/2014JB011708