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Phase Relations in the MgSiO3 System Associated With Hot Mantle Upwelling Across the 660 km Depth
The phase transformations of MgSiO3 bridgmanite control the structure, dynamics and chemistry of the Earth's mantle. Formation of bridgmanite occurs at a depth of about 660 km causing the strong and abrupt seismic discontinuity. Previous experimental studies have revealed that this discontinuity is
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