Major softening at brittle‐ductile transition due to interplay between chemical and deformation processes: An insight from evolution of shear bands in the South Armorican Shear Zone-Reference-Cited by-同舟云学术

Major softening at brittle‐ductile transition due to interplay between chemical and deformation processes: An insight from evolution of shear bands in the South Armorican Shear Zone

Published:2016-02 Issue:2 Volume:121 Page:1158-1182
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Bukovská Zita¹²,Jeřábek Petr¹,Morales Luiz F. G.³

Affiliation:

1. Institute of Petrology and Structural GeologyCharles University in Prague Prague Czech Republic

2. Czech Geological Survey Prague Czech Republic

3. Helmholtz Centre Potsdam, German Research Centre GFZ Potsdam Germany

Funder

Grantová Agentura, Univerzita Karlova

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015JB012319

Reference98 articles.

1. Shear band formation and strain localization on a regional scale: Evidence from anisotropic rocks below a major detachment (Betic Cordilleras, Spain)

2. Titanium in phengite: a geobarometer for high temperature eclogites

3. Palaeozoic history of the Armorican Massif: Models for the tectonic evolution of the suture zones

4. Brittle faults are weak, yet the ductile middle crust is strong: Implications for lithospheric mechanics

5. The generation of plate tectonics from mantle convection

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