201. Editorial for Special Issue "High-Pressure Physical and Chemical Behaviors of Minerals and Rocks".
- Author
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Dai, Lidong and Hu, Haiying
- Subjects
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INTERNAL structure of the Earth , *MINERALS , *EARTH sciences , *HYDROXIDE minerals , *SILICATE minerals , *SMALL-angle neutron scattering - Abstract
Furthermore, the pressure-temperature diagram in the phase boundary of calcite was well established at temperature ranges from 298 K to 773 K, pressures up to 16.0 GPa, and a depth up to 480 km, and further, its potential geophysical implications were discussed in detail. At three representative pressure points (i.e., 10.5 GPa, 12.5 GPa, and 13.8 GPa), the phase transition temperatures between CaCO SB 3 sb -III and CaCO SB 3 sb -VI phases were individually determined. They found that the high-pressure hematite phase began to form at the temperature point of 653 K and, subsequently, the starting material of the pyrite phase was thoroughly transformed into the hematite phase at the temperature point of 688 K, and, finally, the hematite phase would be melted at a temperature higher than 853 K. [Extracted from the article]
- Published
- 2023
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