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.
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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- Formation of Nanocrystalline and Amorphous Materials Causes Parallel Brittle‐Viscous Flow of Crustal Rocks: Experiments on Quartz‐Feldspar Aggregates M. Pec & S. Al Nasser
- Deformation at low and high stress-loading rates C. Trepmann & L. Seybold
- Weak and Slow, Strong and Fast: How Shear Zones Evolve in a Dry Continental Crust (Musgrave Ranges, Central Australia) F. Hawemann et al.
- Dominant slip systems of quartz under lower amphibolite-facies conditions identified from microstructures and CPOs in quartz phenocrysts Q. Wang et al.
- P-T-t-d constraints on post-orogenic deformation and coeval mineralisation in the Archean-Paleoproterozoic transition zone of the southern West African Craton J. Perret et al.
- Interplay between seismic fracture and aseismic creep in the Woodroffe Thrust, central Australia – Inferences for the rheology of relatively dry continental mid-crustal levels S. Wex et al.
- Fluid-enhanced grain-size reduction of K-feldspar from a natural middle crustal shear zone in northern Beijing, China B. Zhou et al.
- Investigating the generation of transport-parallel gradients in ductile strain and kinematic vorticity in the footwalls of metamorphic core complexes: Insights from the Northern Snake Range, Nevada, USA A. Rosenberger et al.
- Petrofabric and Raman microspectroscopy study of the Mina Afortunada gneiss dome: Mapping its thermal gradient P. Puelles & B. Ábalos
- Preferred Orientation of Quartz in Metamorphic Rocks from the Bergell Alps H. Wenk et al.
- A Multiscale Numerical Modeling Investigation on the Significance of Flow Partitioning for the Development of Quartz c‐Axis Fabrics A. Bhandari & D. Jiang
- Spherulitic and rotational crystal growth of Quartz thin films N. Lutjes et al.
- A review of phyllosilicate LPOs: insights from antigorite and chlorite D. Kim & M. Park
- Mechanical properties and recrystallization of quartz in presence of H2O: Combination of cracking, subgrain rotation and dissolution-precipitation processes P. Pongrac et al.
- High-stress creep preceding coseismic rupturing in amphibolite-facies ultramylonites S. Papa et al.
- Temperature and strain controls on ice deformation mechanisms: insights from the microstructures of samples deformed to progressively higher strains at −10, −20 and −30 °C S. Fan et al.
- Porosity induced by dislocation dynamics in quartz-rich shear bands of granitic rocks J. Précigout et al.
- Deformation of feldspar at greenschist facies conditions – the record of mylonitic pegmatites from the Pfunderer Mountains, Eastern Alps F. Hentschel et al.
- Hydrolytic weakening controls Jurassic to early Cretaceous mylonitisation in the basement of the Pyrenees E. González-Esvertit et al.
- Deformation mechanisms and rheology inversion of jointly deformed marble and quartzite in natural thermal gradient K. Schulmann et al.
- Quartz textural analysis from an anastomosing shear zone system: Implications for the tectonic evolution of the Ribeira belt, Brazil T. Conte et al.
- Lattice preferred orientation of quartz in granitic gneisses from Tso Morari Crystalline Complex, Eastern Ladakh, trans-Himalaya: evaluating effect of Dauphiné twin in dynamic recrystallization during exhumation A. Dey et al.
- The brittle-to-viscous transition in polycrystalline quartz: An experimental study B. Richter et al.
- Stresses during pseudotachylyte formation - Evidence from deformed amphibole and quartz in fault rocks from the Silvretta basal thrust (Austria) L. Brückner & C. Trepmann
- 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.
- Strain localization in quartzo-feldspathic mylonites from Patos shear zone revealed by EBSD data M. Alves da Silva et al.
- Magmatic and solid-state flow of a 3.3 Ga rhyolite from the Gavião Block, São Francisco Craton, Brazil F. Braga de Oliveira et al.
- Assessment of Quartz Grain Growth and the Application of the Wattmeter to Predict Quartz Recrystallized Grain Sizes L. Tokle & G. Hirth
- Relation between finite strain geometry and quartz petrofabrics in a folded conglomerate in the Norwegian Caledonides S. Jaensch et al.
- Deformation of Fine‐Grained Quartz Aggregates by Mixed Diffusion and Dislocation Creep J. Fukuda et al.
- Quartz microstructures and crystallographic preferred orientation analysis across the Himalayan metamorphic core reveal exhumation through changing taper angle and strain partitioning along discreet fault zones A. Sen et al.
- Dominant Slip Systems in Quartz and Their Effects on Continental Crust Rheology T. OKUDAIRA
- Comment on “Quartz grainsize evolution during dynamic recrystallization across a natural shear zone boundary” by Haoran Xia and John P. Platt M. Stipp
- Thermometry and Microstructural Analysis Imply Protracted Extensional Exhumation of the Tso Morari UHP Nappe, Northwestern Himalaya: Implications for Models of UHP Exhumation S. Long et al.
- Flow laws and fabric transitions in wet quartzite L. Tokle et al.
- Deformation mechanisms accommodating progressive simple shear thrusting of quartzite and metacarbonate in the southwestern Espinhaço Range, Brazil R. Taufner et al.
- Extracting quartz deformation fabrics from polymineralic rocks G. Casale et al.
- Tectono-magmatic evolution of the Amet granite-gneiss terrane, Sandmata Complex (NW India): Implications for Paleoproterozoic crustal accretion during Columbia assembly M. Sahu et al.
- GGR Biennial Critical Review: Analytical Developments Since 2014 K. Linge et al.
- Effect of pressure on the deformation of quartz aggregates in the presence of H2O L. Nègre et al.
- Quartz porosity in amorphous SiO2 of granitic shear bands J. Précigout et al.
- Transient deformation and long-term tectonic activity in the Eastern Alps recorded by mylonitic pegmatites F. Hentschel et al.
- The application and associated problems of EBSD technique in fabric analysis Z. Qing & L. Xin
- Timing and duration of meteoric water infiltration in the Quiberon detachment zone (Armorican Massif, Variscan belt, France) C. Dusséaux et al.
- Slab kinematics and strain localization in NE China: Polyphase deformation of the Hulin Complex during Late Mesozoic subduction W. Pi et al.
- The structural evolution of the Qomolangma Formation, Mount Everest, Nepal K. Larson et al.
- Calcite fabric development in calc-mylonite during progressive shallowing of a shear zone: An example from the South Tibetan Detachment system (Kali Gandaki valley, Central Himalaya) L. Nania et al.
- The temperature change shortcut: effects of mid-experiment temperature changes on the deformation of polycrystalline ice L. Craw et al.
- Engineering Multiple Microstructural Defects for Record‐Breaking Thermoelectric Properties of Chalcopyrite Cu1‐xAgxGaTe2 L. Huang et al.
- Shear localization in polycrystalline metal at high-strain rates with dynamic recrystallization: Crystal plasticity modeling and texture effect W. An et al.
- Texture and Shape Analysis of Quartzite Mylonites of the Metamorphic Sole of the Samail Ophiolite (Oman): Evidence for Syn- and Post-Obduction Deformation P. Hallas & W. Bauer
Saved (final revised paper)
Latest update: 11 May 2026
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...