Abstract
Experiments were carried out to account for the transformation plasticity for pure ice subjected to isothermal pressure cycling between ice I and II, while simultaneously experiencing a small uniaxial compressive stress. Results of the study shed light on geological materials for which pressure-induced transformation plasticity cannot be reproduced experimentally in the laboratory.
Original language | English (US) |
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Pages (from-to) | 668-671 |
Number of pages | 4 |
Journal | Physical review letters |
Volume | 86 |
Issue number | 4 |
DOIs | |
State | Published - Jan 22 2001 |
ASJC Scopus subject areas
- General Physics and Astronomy