Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean

Seismic observation of ULVZs and LLVP edges. a Seismic shear-wave

Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean

Structure, Materials and Processes in the Earth's Core and Mantle

Origins of ultralow velocity zones through slab-derived metallic melt

SE - Timescales of chemical equilibrium between the convecting solid mantle and over- and underlying magma oceans

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

Lowermost Mantle Structure Beneath the Central Pacific Ocean: Ultralow Velocity Zones and Seismic Anisotropy - Wolf - 2023 - Geochemistry, Geophysics, Geosystems - Wiley Online Library

Globally distributed subducted materials along the Earth's core-mantle boundary: Implications for ultralow velocity zones

Lowermost Mantle Structure Beneath the Central Pacific Ocean: Ultralow Velocity Zones and Seismic Anisotropy - Wolf - 2023 - Geochemistry, Geophysics, Geosystems - Wiley Online Library

Investigating ultra-low velocity zones in the southern hemisphere using an Antarctic dataset - ScienceDirect

PDF] Tracking deep mantle reservoirs with ultra-low velocity zones