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 Kolkata
Categories
Mineral Physics, Phase Transition, Plate Dynamics in Subduction Zone
Funding
Indian Institute of Science Education and Research Kolkata
Science and Engineering Research Board
SRG/2021/001665