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I will present on the kinetic boundary for the transformation of ice I into nearby high-pressure water ices,which was determined at 0-3 GPa and 80-210 K,by means of Raman spectroscopy and diamond anvil cells.In particular,at 80K and 100 K,ice I transformed to high density amorphous ice(HDA),[1] which in turn crystallized into ice Ⅶ upon further compression above 4 GPa and 2 GPa,respectively.