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Volume 8, issue 5
Solid Earth, 8, 1095–1117, 2017
https://doi.org/10.5194/se-8-1095-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

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

Solid Earth, 8, 1095–1117, 2017
https://doi.org/10.5194/se-8-1095-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 25 Oct 2017

Research article | 25 Oct 2017

Analysis of crystallographic preferred orientations of experimentally deformed Black Hills Quartzite

Rüdiger Kilian and Renée Heilbronner Rüdiger Kilian and Renée Heilbronner
  • Department of Environmental Sciences, Geological Institute, Bernoullistrasse 32, 4056 Basel, Switzerland

Abstract. The crystallographic preferred orientations (textures) of three samples of Black Hills Quartzite (BHQ) deformed experimentally in the dislocation creep regimes 1, 2 and 3 (according to Hirth and Tullis, 1992) have been analyzed using electron backscatter diffraction (EBSD). All samples were deformed to relatively high strain at temperatures of 850 to 915 °C and are almost completely dynamically recrystallized. A texture transition from peripheral [c] axes in regime 1 to a central [c] maximum in regime 3 is observed. Separate pole figures are calculated for different grain sizes, aspect ratios and long-axis trends of grains, and high and low levels of intragranular deformation intensity as measured by the mean grain kernel average misorientation (gKAM). Misorientation relations are analyzed for grains of different texture components (named Y, B, R and σ grains, with reference to previously published prism, basal, rhomb and σ1 grains). Results show that regimes 1 and 3 correspond to clear end-member textures, with regime 2 being transitional. Texture strength and the development of a central [c]-axis maximum from a girdle distribution depend on deformation intensity at the grain scale and on the contribution of dislocation creep, which increases towards regime 3. Adding to this calculations of resolved shear stresses and misorientation analysis, it becomes clear that the peripheral [c]-axis maximum in regime 1 is not due to deformation by basal 〈a〉 slip. Instead, we interpret the texture transition as a result of different texture forming processes, one being more efficient at high stresses (nucleation or growth of grains with peripheral [c] axes), the other depending on strain (dislocation glide involving prism and rhomb 〈a〉 slip systems), and not as a result of temperature-dependent activity of different slip systems.

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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...
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