Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean
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Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean
Geology: Chemical leftovers from Earth's formation 4.5 billion years ago may sit near planet's core
SE - Timescales of chemical equilibrium between the convecting solid mantle and over- and underlying magma oceans
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Investigating ultra-low velocity zones in the southern hemisphere using an Antarctic dataset - ScienceDirect
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Improved Characterization of Ultralow‐Velocity Zones Through Advances in Bayesian Inversion of ScP Waveforms - Pachhai - 2023 - Journal of Geophysical Research: Solid Earth - Wiley Online Library
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PDF] Tracking deep mantle reservoirs with ultra-low velocity zones
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PDF] Tracking deep mantle reservoirs with ultra-low velocity zones
Improved Characterization of Ultralow‐Velocity Zones Through Advances in Bayesian Inversion of ScP Waveforms - Pachhai - 2023 - Journal of Geophysical Research: Solid Earth - Wiley Online Library
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