Abstract
Recent structural study of the high-pressure Zn2SiO4 phases III and IV has suggested that they are retrograde phases formed during decompression. To clarify the stabilities of these phases under pressure, in-situ high- pressure Raman spectroscopic measurements were taken at room temperature. Phase III, having a 'tetrahedral olivine' structure, transformed to a new phase at 5.5 GPa during compression and returned to phase III at 1.7 GPa during decompression. Phase IV also exhibited a phase transition at 2.5 GPa with very small hysteresis. Both transitions are first-order. These observations confirmed that phases III and IV are retrograde phases.
Original language | English |
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Pages (from-to) | 263-267 |
Number of pages | 5 |
Journal | Journal of Mineralogical and Petrological Sciences |
Volume | 113 |
Issue number | 5 |
DOIs | |
Publication status | Published - 2018 |
Keywords
- High-pressure phase
- Phase transition
- Raman spectroscopy
- Unquenchable phase
- ZnSiO
ASJC Scopus subject areas
- Geophysics
- Geology