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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Published in | Geochemistry, geophysics, geosystems : G3 Vol. 26; no. 3 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
Washington
John Wiley & Sons, Inc
01.03.2025
Wiley |
Subjects | |
Online Access | Get full text |
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