It is generally recognized that the fabric pattern of ice in polar ice sheets gradually changes from the random pattern to characteristic ones as the single maximum or the small circle girdle according to increase of the depth. We have considered three main mechanisms for the development of the ice fabric, 1) rotation of basal plane acompanied by deformation 2) grain groth 3) recrystallization. With respect to the mechanism 1), we obtained a quantitative relationship between the rotation angle of c-axis of individual grains in compressed polycrystalline ice and the amount of uniaxial strain by experiments, and the obtained result of concentration tendency of c-axes with increasing strain was successfully applied to the observed fabric chang...
In this contribution we present a review of the evolution of microstructures and fabric in ice. Base...
Results of numerical simulations of co-axial deformation of pure ice up to high-strain, combining fu...
Ice is a common mineral at the Earth’s surface. How much ice is stored in the Greenland and Antarcti...
Flow behavior of large ice sheets is affected mainly by c-axis orientation fabric, and the fabric fo...
Abstract: The deformation and recrystallization mechanisms which control the viscoplasticity of ice ...
Creep tests were performed in torsion on polycrystalline ice at temperatures near the melting point....
The deformation and recrystallization mechanisms which control the viscoplasticity of ice from polar...
Crystallographic investigations have been conducted of cold (-17°C) debris-bearing ice from the base...
Optical orientation of approximately 5000 ice crystals was determined on the Emmons Glacier in 1950,...
We propose a new method to investigate the relationships between neighbouring crystals and apply it ...
International audienceTorsion experiments were performed in polycrys-talline ice at high temperature...
Microstructural analyses have been performed on polar firn from the European Project for Ice Coring ...
International audienceDynamic recrystallization (DRX) occurs in minerals, metals, ice and impact on ...
The primary objective of this thesis is the investigation of microstructures obtained from samples f...
In this contribution we present a review of the evolution of microstructures and fabric in ice. Base...
In this contribution we present a review of the evolution of microstructures and fabric in ice. Base...
Results of numerical simulations of co-axial deformation of pure ice up to high-strain, combining fu...
Ice is a common mineral at the Earth’s surface. How much ice is stored in the Greenland and Antarcti...
Flow behavior of large ice sheets is affected mainly by c-axis orientation fabric, and the fabric fo...
Abstract: The deformation and recrystallization mechanisms which control the viscoplasticity of ice ...
Creep tests were performed in torsion on polycrystalline ice at temperatures near the melting point....
The deformation and recrystallization mechanisms which control the viscoplasticity of ice from polar...
Crystallographic investigations have been conducted of cold (-17°C) debris-bearing ice from the base...
Optical orientation of approximately 5000 ice crystals was determined on the Emmons Glacier in 1950,...
We propose a new method to investigate the relationships between neighbouring crystals and apply it ...
International audienceTorsion experiments were performed in polycrys-talline ice at high temperature...
Microstructural analyses have been performed on polar firn from the European Project for Ice Coring ...
International audienceDynamic recrystallization (DRX) occurs in minerals, metals, ice and impact on ...
The primary objective of this thesis is the investigation of microstructures obtained from samples f...
In this contribution we present a review of the evolution of microstructures and fabric in ice. Base...
In this contribution we present a review of the evolution of microstructures and fabric in ice. Base...
Results of numerical simulations of co-axial deformation of pure ice up to high-strain, combining fu...
Ice is a common mineral at the Earth’s surface. How much ice is stored in the Greenland and Antarcti...