What it is
In this study, we map water content at the MTZ base by combining mineral physics constraints on hydrous pyrolite and global seismic observations of velocity structure and 660-km discontinuity topography. Our results indicate an average global water content of approximately 0.14 wt%, with pronounced hydration anomalies in parts of Asia.
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Filed underHigh-pressure geophysics and materials, Geological and Geochemical Analysis, Astro and Planetary Science