Strain rate dependence for evolution of steady state grain sizes: Insights from high-strain experiments on ice-Reference-Cited by-同舟云学术

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Strain rate dependence for evolution of steady state grain sizes: Insights from high-strain experiments on ice

Published:2019-01 Issue: Volume:506 Page:168-174
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Peternell Mark,Wilson Christopher J.L.,Hammes Daniel M.

Funder

Antarctic Science Advisory Committee

Australian Research Council

VAMOS

IAMG Computers and Geosciences Scholarship 2015

Sibylle Kalkhof-Rose Stiftung

DAAD-Australia–Germany Joint Research Co-operation Scheme

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference37 articles.

1. A flow law for anisotrophic polycrystalline ice under uniaxial compressive deformation;Azuma;Cold Reg. Sci. Technol.,1995

2. A review of ice rheology for ice sheet modelling;Budd;Cold Reg. Sci. Technol.,1989

3. Non-basal dislocations should be accounted for in simulating ice mass flow;Chauve;Earth Planet. Sci. Lett.,2017

4. A phenomenological numerical approach for investigating grain size evolution in ductiley deforming rocks;Cross;J. Struct. Geol.,2015

5. On dynamic recrystallization during solid state flow: effects of stress and temperature;De Bresser;Geophys. Res. Lett.,1998

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2. Study on mechanical properties and constitutive model for polycrystalline ice samples;Environmental Earth Sciences;2023-11-21

3. The temperature change shortcut: effects of mid-experiment temperature changes on the deformation of polycrystalline ice;The Cryosphere;2021-05-10

4. 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;The Cryosphere;2020-07-27

5. Deformation of polycrystalline D2O ice: Its sensitivity to temperature and strain-rate as an analogue for terrestrial ice;Earth and Planetary Science Letters;2020-02

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