Articles | Volume 8, issue 5
https://doi.org/10.5194/se-8-1095-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/se-8-1095-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Analysis of crystallographic preferred orientations of experimentally deformed Black Hills Quartzite
Rüdiger Kilian
CORRESPONDING AUTHOR
Department of Environmental Sciences, Geological Institute, Bernoullistrasse
32, 4056 Basel, Switzerland
Renée Heilbronner
Department of Environmental Sciences, Geological Institute, Bernoullistrasse
32, 4056 Basel, Switzerland
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42 citations as recorded by crossref.
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- Weak and Slow, Strong and Fast: How Shear Zones Evolve in a Dry Continental Crust (Musgrave Ranges, Central Australia) F. Hawemann et al. 10.1029/2018JB016559
- Role of pre-kinematic fluid-rock interactions on phase mixing, quartz recrystallization and strain localization in low-temperature granitic shear zones K. Alaoui et al. 10.1016/j.tecto.2023.229735
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- Relation between finite strain geometry and quartz petrofabrics in a folded conglomerate in the Norwegian Caledonides S. Jaensch et al. 10.1016/j.jsg.2022.104604
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Discussed (final revised paper)
Discussed (preprint)
Latest update: 20 Nov 2024
Short summary
Quartz crystallographic preferred orientations (textures) are widely used to interpret conditions, kinematics or deformation mechanisms in deformed rocks. Textures of experimentally deformed quartzite were analyzed and we find that the finite texture is the result of two different texture-forming processes that depend on stress and strain but not directly on temperature. The findings help in the interpretation of deformation conditions from textures in naturally deformed rocks.
Quartz crystallographic preferred orientations (textures) are widely used to interpret...