Effect of Fe2+ on akimotoite to bridgmanite transition: Its implication on subduction dynamics (data)
Published: 11 September 2024| Version 1 | DOI: 10.17632/w2b25bb7dv.1
Contributors:
P Pandit, , Description
1. Cell parameters and volumes nearly at 0 GPa pressure 2. Birch–Murnaghan's 3rd order equation fitting parameters 3.Phase transition pressures and temperatures for different Fe2+ concentration along mantle geotherm and cold slab geotherms using LDA/GGA+U methods 4.Calculated thermal elastic constants (GPa) of structures 5.Calculated thermal volume (V), bulk modulus (K), and shear modulus (G) of structures
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Institutions
- Indian Institute of Science Education and Research KolkataWest Bengal, Mohanpur
Categories
Mineral Physics, Phase Transition, Plate Dynamics in Subduction Zone
Funders
- Indian Institute of Science Education and Research KolkataWest Bengal, India