Non-Basal Slip as a Major Deformation Process in the Creep of Polycrystalline Ice

Abstract Published data on the creep of polycrystalline ice and crystals oriented for non-basal slip are discussed in terms of theories of prismatic slip in hexagonal metals. It is concluded that creep of polycrystalline ice near the melting point is controlled by non-basal slip but a decision on th...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Tegart, W. J. McG.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1964
Subjects:
Earth-Surface Processes
Journal of Glaciology
Online Access:http://dx.doi.org/10.1017/s0022143000028859
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000028859
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spelling crcambridgeupr:10.1017/s0022143000028859 2024-03-03T08:46:04+00:00 Non-Basal Slip as a Major Deformation Process in the Creep of Polycrystalline Ice Tegart, W. J. McG. 1964 http://dx.doi.org/10.1017/s0022143000028859 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000028859 en eng Cambridge University Press (CUP) Journal of Glaciology volume 5, issue 38, page 251-254 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1964 crcambridgeupr https://doi.org/10.1017/s0022143000028859 2024-02-08T08:36:15Z Abstract Published data on the creep of polycrystalline ice and crystals oriented for non-basal slip are discussed in terms of theories of prismatic slip in hexagonal metals. It is concluded that creep of polycrystalline ice near the melting point is controlled by non-basal slip but a decision on the exact mechanism of slip cannot be made on the basis of available data. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 5 38 251 254
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Tegart, W. J. McG.
Non-Basal Slip as a Major Deformation Process in the Creep of Polycrystalline Ice
topic_facet Earth-Surface Processes
description Abstract Published data on the creep of polycrystalline ice and crystals oriented for non-basal slip are discussed in terms of theories of prismatic slip in hexagonal metals. It is concluded that creep of polycrystalline ice near the melting point is controlled by non-basal slip but a decision on the exact mechanism of slip cannot be made on the basis of available data.
format Article in Journal/Newspaper
author Tegart, W. J. McG.
author_facet Tegart, W. J. McG.
author_sort Tegart, W. J. McG.
title Non-Basal Slip as a Major Deformation Process in the Creep of Polycrystalline Ice
title_short Non-Basal Slip as a Major Deformation Process in the Creep of Polycrystalline Ice
title_full Non-Basal Slip as a Major Deformation Process in the Creep of Polycrystalline Ice
title_fullStr Non-Basal Slip as a Major Deformation Process in the Creep of Polycrystalline Ice
title_full_unstemmed Non-Basal Slip as a Major Deformation Process in the Creep of Polycrystalline Ice
title_sort non-basal slip as a major deformation process in the creep of polycrystalline ice
publisher Cambridge University Press (CUP)
publishDate 1964
url http://dx.doi.org/10.1017/s0022143000028859
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000028859
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 5, issue 38, page 251-254
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000028859
container_title Journal of Glaciology
container_volume 5
container_issue 38
container_start_page 251
op_container_end_page 254
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