Effect of Fe2+ on Akimotoite to Bridgmanite Transition: Its Implication on Subduction Dynamics

Seismic studies in cold subduction zones indicate several discontinuity structures near the 660‐km boundary. Studies indicate that the akimotoite to bridgmanite transition may play a significant role in unraveling the complexity of this region. In this study, we used first‐principles methods to expl...

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Bibliographic Details
Published inGeochemistry, geophysics, geosystems : G3 Vol. 26; no. 3
Main Authors Pandit, Priyanka, Chandrashekhar, Prathibha, Sharma, Sparsh, Shukla, Gaurav
Format Journal Article
LanguageEnglish
Published Washington John Wiley & Sons, Inc 01.03.2025
Wiley
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