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

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

Thermodynamical constraints on the crystallization of a deep magma-ocean on Earth - ScienceDirect

Magma oceans as a critical stage in the tectonic development of rocky planets Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences

Origins of ultralow velocity zones through slab-derived metallic melt

Magma ocean solidification. (a) Initiation of mantle crystallization

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

Compositional and thermal state of the lower mantle from joint 3D inversion with seismic tomography and mineral elasticity

Origins of ultralow velocity zones through slab-derived metallic melt

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

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