32 citations as recorded by crossref.

1. Kinking facilitates grain nucleation and modifies crystallographic preferred orientations during high-stress ice deformation S. Fan et al. 10.1016/j.epsl.2021.117136
2. Can changes in deformation regimes be inferred from crystallographic preferred orientations in polar ice? M. Llorens et al. 10.5194/tc-16-2009-2022
3. A stratigraphy-based method for reconstructing ice core orientation J. Westhoff et al. 10.1017/aog.2020.76
4. Crystallographic analysis of temperate ice on Rhonegletscher, Swiss Alps S. Hellmann et al. 10.5194/tc-15-677-2021
5. Melt in the Greenland EastGRIP ice core reveals Holocene warm events J. Westhoff et al. 10.5194/cp-18-1011-2022
6. Physical analysis of an Antarctic ice core—towards an integration of micro- and macrodynamics of polar ice I. Weikusat et al. 10.1098/rsta.2015.0347
7. 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
8. Folds inside pebbles: When do they form during conglomerate deformation? Numerical modelling and comparison with the Hutuo Group conglomerates, North China Craton H. Ran et al. 10.1016/j.jsg.2022.104620
9. Stress and strain evolution during single-layer folding under pure and simple shear M. Llorens 10.1016/j.jsg.2019.06.009
10. High-strain deformation of conglomerates: Numerical modelling, strain analysis, and an example from the Wutai Mountains, North China Craton H. Ran et al. 10.1016/j.jsg.2018.06.018
11. EBSD analysis of subgrain boundaries and dislocation slip systems in Antarctic and Greenland ice I. Weikusat et al. 10.5194/se-8-883-2017
12. The Relevance of Grain Dissection for Grain Size Reduction in Polar Ice: Insights from Numerical Models and Ice Core Microstructure Analysis F. Steinbach et al. 10.3389/feart.2017.00066
13. Dynamic recrystallization during deformation of polycrystalline ice: insights from numerical simulations M. Llorens et al. 10.1098/rsta.2015.0346
14. Impurity Analysis and Microstructure Along the Climatic Transition From MIS 6 Into 5e in the EDML Ice Core Using Cryo-Raman Microscopy J. Eichler et al. 10.3389/feart.2019.00020
15. Development of crystal orientation fabric in the Dome Fuji ice core in East Antarctica: implications for the deformation regime in ice sheets T. Saruya et al. 10.5194/tc-16-2985-2022
16. The IceCube Neutrino Observatory: instrumentation and online systems M. Aartsen et al. 10.1088/1748-0221/12/03/P03012
17. Time for anisotropy: The significance of mechanical anisotropy for the development of deformation structures H. Ran et al. 10.1016/j.jsg.2018.04.019
18. Two-dimensional impurity imaging in deep Antarctic ice cores: snapshots of three climatic periods and implications for high-resolution signal interpretation P. Bohleber et al. 10.5194/tc-15-3523-2021
19. Using a composite flow law to model deformation in the NEEM deep ice core, Greenland – Part 1: The role of grain size and grain size distribution on deformation of the upper 2207 m E. Kuiper et al. 10.5194/tc-14-2429-2020
20. Using a composite flow law to model deformation in the NEEM deep ice core, Greenland – Part 2: The role of grain size and premelting on ice deformation at high homologous temperature E. Kuiper et al. 10.5194/tc-14-2449-2020
21. Predicting the steady-state isochronal stratigraphy of ice shelves using observations and modeling V. Višnjević et al. 10.5194/tc-16-4763-2022
22. Strain localization and dynamic recrystallization in the ice–air aggregate: a numerical study F. Steinbach et al. 10.5194/tc-10-3071-2016
23. Greenland Ice Sheet: Higher Nonlinearity of Ice Flow Significantly Reduces Estimated Basal Motion P. Bons et al. 10.1029/2018GL078356
24. Electrical stratigraphy of the WAIS Divide ice core: Identification of centimeter‐scale irregular layering T. Fudge et al. 10.1002/2016JF003845
25. A review of numerical modelling of the dynamics of microstructural development in rocks and ice: Past, present and future S. Piazolo et al. 10.1016/j.jsg.2018.05.025
26. Holocene ice-stream shutdown and drainage basin reconfiguration in northeast Greenland S. Franke et al. 10.1038/s41561-022-01082-2
27. Crystallographic Preferred Orientation (CPO) Development Governs Strain Weakening in Ice: Insights From High‐Temperature Deformation Experiments S. Fan et al. 10.1029/2021JB023173
28. Converging flow and anisotropy cause large-scale folding in Greenland's ice sheet P. Bons et al. 10.1038/ncomms11427
29. Strain field evolution at the ductile-to-brittle transition: a case study on ice T. Chauve et al. 10.5194/se-8-943-2017
30. Full-field predictions of ice dynamic recrystallisation under simple shear conditions M. Llorens et al. 10.1016/j.epsl.2016.06.045
31. Crystallographic preferred orientations of ice deformed in direct-shear experiments at low temperatures C. Qi et al. 10.5194/tc-13-351-2019
32. Microstructural analysis of Greenland ice using a cryogenic scanning electron microscope equipped with an electron backscatter diffraction detector W. SHIGEYAMA et al. 10.5331/bgr.19R01