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...
Published in: | Journal of Glaciology |
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Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
1964
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Subjects: | |
Online Access: | http://dx.doi.org/10.1017/s0022143000028859 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000028859 |
Summary: | 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. |
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