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

Slab control on the mega-sized North Pacific ultra-low velocity zone

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

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

Mysterious Zone Between Earth's Inner Core and Mantle an Effect of Interplanetary Collision 4.5 Billion Years Ago

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

Geology: Chemical leftovers from Earth's formation 4.5 billion years ago may sit near planet's core

PDF) Origins of ultralow velocity zones through slab-derived metallic melt

Geology: Chemical leftovers from Earth's formation 4.5 billion years ago may sit near planet's core

Subducted oceanic crust as the origin of seismically slow lower-mantle structures, Progress in Earth and Planetary Science