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Solid Earth An interactive open-access journal of the European Geosciences Union
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Short summary
The crystallographic texture of experimentally sheared samples of dynamically recrystallized quartzite have been reanalyzed using EBSD. Detailed grain size analysis reveals that the recrystallized grain size depends not only on stress, as assumed in the recrystallized quartz piezometer of Stipp and Tullis (2003), but also on texture, grain-scale deformation intensity, and the kinematic framework of axial versus general shear experiments.
Articles | Volume 8, issue 5
Solid Earth, 8, 1071–1093, 2017
https://doi.org/10.5194/se-8-1071-2017

Special issue: Analysis of deformation microstructures and mechanisms on...

Solid Earth, 8, 1071–1093, 2017
https://doi.org/10.5194/se-8-1071-2017

Research article 17 Oct 2017

Research article | 17 Oct 2017

The grain size(s) of Black Hills Quartzite deformed in the dislocation creep regime

Renée Heilbronner and Rüdiger Kilian

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Short summary
The crystallographic texture of experimentally sheared samples of dynamically recrystallized quartzite have been reanalyzed using EBSD. Detailed grain size analysis reveals that the recrystallized grain size depends not only on stress, as assumed in the recrystallized quartz piezometer of Stipp and Tullis (2003), but also on texture, grain-scale deformation intensity, and the kinematic framework of axial versus general shear experiments.
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