Pressure-Induced Reverse Structural Transition of Calcite at Temperatures up to 873 K and Pressures up to 19.7 GPa

نویسندگان

چکیده

In situ Raman scattering and electrical conductivity experiments have been performed to investigate the structural phase transitions of calcite during compressed decompressed processes in a diamond anvil cell at temperatures 298–873 K pressures up 19.7 GPa. Upon compression, (CaCO3-I phase) underwent three from CaCO3-I CaCO3-II phases 1.6 GPa, CaCO3-III 2.2 CaCO3-VI 16.8 GPa under room temperature conditions, which were evidenced by evolution peaks, as well discontinuities pressure-dependent shifts conductivity. decompression, took place respective 5.4, 1.5, 0.4 indicating reversibility calcite. Furthermore, an obvious ~11 pressure hysteresis was detected transition, whereas other reverse transition very close those results. At given representative conditions (i.e., 10.5, 12.5, 13.8 GPa), series ranges 323–873 explore temperature-dependent relation transition. With increasing pressure, between gradually decreases, reveals obviously negative temperature-pressure relation, i.e., P (GPa) = 19.219 (±1.105) − 0.011 (±0.002) T (K). Our acquired diagram can be employed understand high-pressure stability for carbonate minerals along various subducting slabs deep Earth’s interior.

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ژورنال

عنوان ژورنال: Minerals

سال: 2023

ISSN: ['2075-163X']

DOI: https://doi.org/10.3390/min13020188