Articles | Volume 13, issue 5
https://doi.org/10.5194/tc-13-1495-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-13-1495-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Recrystallization processes, microstructure and crystallographic preferred orientation evolution in polycrystalline ice during high-temperature simple shear
Baptiste Journaux
CORRESPONDING AUTHOR
Department of Earth and Space Sciences, University of Washington, NASA Astrobiology
Institute, Seattle, USA
Université Grenoble Alpes, CNRS, IRD, G-INP, IGE, 38000 Grenoble, France
Thomas Chauve
Université Grenoble Alpes, CNRS, IRD, G-INP, IGE, 38000 Grenoble, France
PGP, Department of Geoscience, University of Oslo, Oslo, Norway
Maurine Montagnat
CORRESPONDING AUTHOR
Université Grenoble Alpes, CNRS, IRD, G-INP, IGE, 38000 Grenoble, France
Andrea Tommasi
Géosciences Montpellier, Université de Montpellier/CNRS, 34095 Montpellier, France
Fabrice Barou
Géosciences Montpellier, Université de Montpellier/CNRS, 34095 Montpellier, France
David Mainprice
Géosciences Montpellier, Université de Montpellier/CNRS, 34095 Montpellier, France
Léa Gest
Université Grenoble Alpes, CNRS, IRD, G-INP, IGE, 38000 Grenoble, France
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26 citations as recorded by crossref.
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- Thrust faulting in glaciers? Re‐examination of debris bands near the margin of Storglaciären, Sweden M. Monz et al. 10.1111/bor.12549
- Tidal Modulation of a Lateral Shear Margin: Priestley Glacier, Antarctica H. Still et al. 10.3389/feart.2022.828313
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- Spatial Variations of Fabric and Microstructure of Blue Ice Cores at the Shear Margin of Dalk Glacier, Antarctica S. Lu et al. 10.3390/w15040728
- Can changes in deformation regimes be inferred from crystallographic preferred orientations in polar ice? M. Llorens et al. 10.5194/tc-16-2009-2022
- Simulating higher-order fabric structure in a coupled, anisotropic ice-flow model: application to Dome C D. Lilien et al. 10.1017/jog.2023.78
- Modeling Ice‐Crystal Fabric as a Proxy for Ice‐Stream Stability D. Lilien et al. 10.1029/2021JF006306
- 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. 10.5194/tc-14-3875-2020
- Softening of Temperate Ice by Interstitial Water C. Adams et al. 10.3389/feart.2021.702761
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- Full crystallographic orientation (<i>c</i> and <i>a</i> axes) of warm, coarse-grained ice in a shear-dominated setting: a case study, Storglaciären, Sweden M. Monz et al. 10.5194/tc-15-303-2021
- Grain growth of natural and synthetic ice at 0 °C S. Fan et al. 10.5194/tc-17-3443-2023
- Multimaxima crystallographic fabrics (CPO) in warm, coarse-grained ice: New insights M. Disbrow-Monz et al. 10.1016/j.jsg.2024.105107
- Investigation of a cold-based ice apron on a high-mountain permafrost rock wall using ice texture analysis and micro-14C dating: a case study of the Triangle du Tacul ice apron (Mont Blanc massif, France) G. Guillet et al. 10.1017/jog.2021.65
- Microstructures in a shear margin: Jarvis Glacier, Alaska C. Gerbi et al. 10.1017/jog.2021.62
- A physically-based formulation for texture evolution during dynamic recrystallization. A case study of ice T. Chauve et al. 10.5802/crmeca.243
- Progresses in Studies on Crystallographic Preferred Orientations in Experimentally Deformed Ice Q. WANG & C. Qi 10.3724/j.issn.1007-2802.20240103
- Microstructure and Crystallographic Preferred Orientations of an Azimuthally Oriented Ice Core from a Lateral Shear Margin: Priestley Glacier, Antarctica R. Thomas et al. 10.3389/feart.2021.702213
- Crystallographic preferred orientation (CPO) patterns in uniaxially compressed deuterated ice: quantitative analysis of historical data N. Hunter et al. 10.1017/jog.2022.95
- Crystallographic preferred orientations of ice deformed in direct-shear experiments at low temperatures C. Qi et al. 10.5194/tc-13-351-2019
25 citations as recorded by crossref.
- Microstructures and Fabric Transitions of Natural Ice from the Styx Glacier, Northern Victoria Land, Antarctica D. Kim et al. 10.3390/min10100892
- Crystallographic analysis of temperate ice on Rhonegletscher, Swiss Alps S. Hellmann et al. 10.5194/tc-15-677-2021
- The evolution of ice fabrics: A continuum modelling approach validated against laboratory experiments D. Richards et al. 10.1016/j.epsl.2020.116718
- Stress sensitivity of high-temperature microstructures in ice, with potential applications to quartz J. Platt et al. 10.1016/j.jsg.2021.104487
- Thrust faulting in glaciers? Re‐examination of debris bands near the margin of Storglaciären, Sweden M. Monz et al. 10.1111/bor.12549
- Tidal Modulation of a Lateral Shear Margin: Priestley Glacier, Antarctica H. Still et al. 10.3389/feart.2022.828313
- Constraining Ice Shelf Anisotropy Using Shear Wave Splitting Measurements from Active‐Source Borehole Seismics F. Lutz et al. 10.1029/2020JF005707
- Ice aprons on steep high-alpine slopes: insights from the Mont-Blanc massif, Western Alps L. Ravanel et al. 10.1017/jog.2023.15
- Ice fabrics in two-dimensional flows: beyond pure and simple shear D. Richards et al. 10.5194/tc-16-4571-2022
- Spatial Variations of Fabric and Microstructure of Blue Ice Cores at the Shear Margin of Dalk Glacier, Antarctica S. Lu et al. 10.3390/w15040728
- Can changes in deformation regimes be inferred from crystallographic preferred orientations in polar ice? M. Llorens et al. 10.5194/tc-16-2009-2022
- Simulating higher-order fabric structure in a coupled, anisotropic ice-flow model: application to Dome C D. Lilien et al. 10.1017/jog.2023.78
- Modeling Ice‐Crystal Fabric as a Proxy for Ice‐Stream Stability D. Lilien et al. 10.1029/2021JF006306
- 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. 10.5194/tc-14-3875-2020
- Softening of Temperate Ice by Interstitial Water C. Adams et al. 10.3389/feart.2021.702761
- Ultrasonic and seismic constraints on crystallographic preferred orientations of the Priestley Glacier shear margin, Antarctica F. Lutz et al. 10.5194/tc-16-3313-2022
- Full crystallographic orientation (<i>c</i> and <i>a</i> axes) of warm, coarse-grained ice in a shear-dominated setting: a case study, Storglaciären, Sweden M. Monz et al. 10.5194/tc-15-303-2021
- Grain growth of natural and synthetic ice at 0 °C S. Fan et al. 10.5194/tc-17-3443-2023
- Multimaxima crystallographic fabrics (CPO) in warm, coarse-grained ice: New insights M. Disbrow-Monz et al. 10.1016/j.jsg.2024.105107
- Investigation of a cold-based ice apron on a high-mountain permafrost rock wall using ice texture analysis and micro-14C dating: a case study of the Triangle du Tacul ice apron (Mont Blanc massif, France) G. Guillet et al. 10.1017/jog.2021.65
- Microstructures in a shear margin: Jarvis Glacier, Alaska C. Gerbi et al. 10.1017/jog.2021.62
- A physically-based formulation for texture evolution during dynamic recrystallization. A case study of ice T. Chauve et al. 10.5802/crmeca.243
- Progresses in Studies on Crystallographic Preferred Orientations in Experimentally Deformed Ice Q. WANG & C. Qi 10.3724/j.issn.1007-2802.20240103
- Microstructure and Crystallographic Preferred Orientations of an Azimuthally Oriented Ice Core from a Lateral Shear Margin: Priestley Glacier, Antarctica R. Thomas et al. 10.3389/feart.2021.702213
- Crystallographic preferred orientation (CPO) patterns in uniaxially compressed deuterated ice: quantitative analysis of historical data N. Hunter et al. 10.1017/jog.2022.95
1 citations as recorded by crossref.
Latest update: 20 Nov 2024
Short summary
Ice mechanics is an important tool to better predict the response of glaciers or polar ice sheets to climate variations.
Nevertheless our current predictive abilities are limited as the microscale mechanisms responsible for ice creep are poorly identified.
We show in this study, using state-of-the-art experimental techniques, which recrystallization processes control ice deformation. This will allow realistic simulations, necessary to predict the long-term effects on ice landmasses.
Ice mechanics is an important tool to better predict the response of glaciers or polar ice...