Can changes in deformation regimes be inferred from crystallographic preferred orientations in polar ice?

<p>Creep due to ice flow is generally thought to be the main cause for the formation of crystallographic preferred orientations (CPOs) in polycrystalline anisotropic ice. However, linking the development of CPOs to the ice flow history requires a proper understanding of the ice aggregate'...

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Bibliographic Details

Published in:	The Cryosphere
Main Authors:	M.-G. Llorens, A. Griera, P. D. Bons, I. Weikusat, D. J. Prior, E. Gomez-Rivas, T. de Riese, I. Jimenez-Munt, D. García-Castellanos, R. A. Lebensohn
Format:	Article
Language:	English
Published:	Copernicus Publications 2022-05-01
Online Access:	https://tc.copernicus.org/articles/16/2009/2022/tc-16-2009-2022.pdf