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Figure 1
P–T phase diagram of water ice. Observed equilibrium phase boundaries are depicted by solid lines, extrapolated equilibrium boundaries by dashed lines. Note that below ∼100 K, ice II can persist metastably up to ∼5 GPa (Song et al., 2003BB43).

Journal logoJOURNAL OF
APPLIED
CRYSTALLOGRAPHY
ISSN: 1600-5767
Volume 38| Part 4| August 2005| Pages 612-618
https://doi.org/10.1107/S0021889805014226
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