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

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