Modelling the mechanical behavior of polycrystalline materials based on their evolving
microstructure and the anisotropic properties of their constituent single crystal grains is …

Understanding the flow of ice in glaciers and polar ice sheets is of increasing relevance in a
time of potentially significant climate change. The flow of ice has hitherto received relatively …

Complexly deformed rocks that exhibit refolded folds and overprinting planar fabrics are
often interpreted as the result of polyphase deformation and described in a scheme of …

This study focused on collecting structural data orientations of a crustal-scale shear zone
(Palmi Shear Zone, PSZ, southern Calabria, Italy,) by integrating various analytical and field …

In this contribution we present a review of the evolution of microstructures and fabric in ice.
Based on the review we show the potential use of ice as an analogue for rocks by …

C′ shear bands are ubiquitous structures in shear zones but their development is poorly
understood. Previous research has determined they mostly occur in rocks with a high …

The flow of glaciers and polar ice sheets is controlled by the highly anisotropic rheology of
ice crystals that have hexagonal symmetry (ice lh). To improve our knowledge of ice sheet …

Understanding the flow of ice on the microstructural scale is essential for improving our
knowledge of large-scale ice dynamics, and thus our ability to predict future changes of ice …

Results of numerical simulations of co-axial deformation of pure ice up to high-strain,
combining full-field modelling with recrystallisation are presented. Grain size and lattice …

Only a few localised ice streams drain most of the ice from the Greenland Ice Sheet. Thus,
understanding ice stream behaviour and its temporal variability is crucially important to …