Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean
Descrição
Possible chemical leftovers from early Earth
Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean
Globally distributed subducted materials along the Earth's core-mantle boundary: Implications for ultralow velocity zones
Magma Ocean, Water, and the Early Atmosphere of Venus
Origins of ultralow velocity zones through slab-derived metallic melt
2022, IN A NUTSHELL
Compositional and thermal state of the lower mantle from joint 3D inversion with seismic tomography and mineral elasticity
Subducted oceanic crust as the origin of seismically slow lower-mantle structures, Progress in Earth and Planetary Science
Lowermost Mantle Structure Beneath the Central Pacific Ocean: Ultralow Velocity Zones and Seismic Anisotropy - Wolf - 2023 - Geochemistry, Geophysics, Geosystems - Wiley Online Library
Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean
PDF] Tracking deep mantle reservoirs with ultra-low velocity zones
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