38 citations as recorded by crossref.

1. 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
2. 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
3. Microstructures in a shear margin: Jarvis Glacier, Alaska C. Gerbi et al. 10.1017/jog.2021.62
4. On the Limitations of Using Polarimetric Radar Sounding to Infer the Crystal Orientation Fabric of Ice Masses N. Rathmann et al. 10.1029/2021GL096244
5. 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
6. 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
7. 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
8. Using grain boundary irregularity to quantify dynamic recrystallization in ice S. Fan et al. 10.1016/j.actamat.2021.116810
9. Macroscopic response and microstructure evolution in viscoplastic polycrystals with pressurized pores S. Das et al. 10.1007/s10704-020-00500-z
10. A physically-based formulation for texture evolution during dynamic recrystallization. A case study of ice T. Chauve et al. 10.5802/crmeca.243
11. Ice fabrics in two-dimensional flows: beyond pure and simple shear D. Richards et al. 10.5194/tc-16-4571-2022
12. Microstructure-sensitive crystal plasticity and phase-field modeling of deformation and fracture in polycrystalline ice S. Motahari et al. 10.1016/j.actamat.2024.120512
13. Multimaxima crystallographic fabrics (CPO) in warm, coarse-grained ice: New insights M. Disbrow-Monz et al. 10.1016/j.jsg.2024.105107
14. Origin of englacial stratigraphy at three deep ice core sites of the Greenland Ice Sheet by synthetic radar modelling S. Mojtabavi et al. 10.1017/jog.2021.137
15. Plastic Faulting in Ice N. Golding et al. 10.1029/2019JB018749
16. Constraining Ice Shelf Anisotropy Using Shear Wave Splitting Measurements from Active‐Source Borehole Seismics F. Lutz et al. 10.1029/2020JF005707
17. Radar Characterization of Ice Crystal Orientation Fabric and Anisotropic Viscosity Within an Antarctic Ice Stream T. Jordan et al. 10.1029/2022JF006673
18. Recrystallization processes, microstructure and crystallographic preferred orientation evolution in polycrystalline ice during high-temperature simple shear B. Journaux et al. 10.5194/tc-13-1495-2019
19. A stratigraphy-based method for reconstructing ice core orientation J. Westhoff et al. 10.1017/aog.2020.76
20. Shear localisation in anisotropic, non-linear viscous materials that develop a CPO: A numerical study T. de Riese et al. 10.1016/j.jsg.2019.03.006
21. The evolution of ice fabrics: A continuum modelling approach validated against laboratory experiments D. Richards et al. 10.1016/j.epsl.2020.116718
22. The temperature change shortcut: effects of mid-experiment temperature changes on the deformation of polycrystalline ice L. Craw et al. 10.5194/tc-15-2235-2021
23. Can changes in deformation regimes be inferred from crystallographic preferred orientations in polar ice? M. Llorens et al. 10.5194/tc-16-2009-2022
24. Crystallographic preferred orientation (CPO) patterns in uniaxially compressed deuterated ice: quantitative analysis of historical data N. Hunter et al. 10.1017/jog.2022.95
25. Microstructures and Fabric Transitions of Natural Ice from the Styx Glacier, Northern Victoria Land, Antarctica D. Kim et al. 10.3390/min10100892
26. Tidal Modulation of a Lateral Shear Margin: Priestley Glacier, Antarctica H. Still et al. 10.3389/feart.2022.828313
27. Does second phase content control the evolution of olivine CPO type and deformation mechanisms? A case study of paired harzburgite and dunite bands in the Red Hills Massif, Dun Mountain Ophiolite Y. Shao et al. 10.1016/j.lithos.2021.106532
28. Bridging the Gap Between Experimental and Natural Fabrics: Modeling Ice Stream Fabric Evolution and its Comparison With Ice‐Core Data D. Richards et al. 10.1029/2023JB027245
29. 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
30. Progresses in Studies on Crystallographic Preferred Orientations in Experimentally Deformed Ice Q. WANG & C. Qi 10.3724/j.issn.1007-2802.20240103
31. Elastic wave propagation in anisotropic polycrystals: inferring physical properties of glacier ice N. Rathmann et al. 10.1098/rspa.2022.0574
32. Strongly Depth‐Dependent Ice Fabric in a Fast‐Flowing Antarctic Ice Stream Revealed With Icequake Observations S. Kufner et al. 10.1029/2022JF006853
33. Cool ice with hot properties S. Fan & D. Prior 10.1038/s41561-023-01330-z
34. Inferring Ice Fabric From Birefringence Loss in Airborne Radargrams: Application to the Eastern Shear Margin of Thwaites Glacier, West Antarctica T. Young et al. 10.1029/2020JF006023
35. Stress sensitivity of high-temperature microstructures in ice, with potential applications to quartz J. Platt et al. 10.1016/j.jsg.2021.104487
36. Modeling the Deformation Regime of Thwaites Glacier, West Antarctica, Using a Simple Flow Relation for Ice Anisotropy (ESTAR) F. McCormack et al. 10.1029/2021JF006332
37. Thrust faulting in glaciers? Re‐examination of debris bands near the margin of Storglaciären, Sweden M. Monz et al. 10.1111/bor.12549
38. Static Ice Pressure Measuring System Based on Fiber Loop Ring-Down Spectroscopy and FPGA X. Deng et al. 10.3390/s20205927