Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean
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PDF) Origins of ultralow velocity zones through slab-derived metallic melt
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
Fractional crystallization of a basal lunar magma ocean: A dense melt-bearing garnetite layer above the core? - ScienceDirect
Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean
Origins of ultralow velocity zones through slab-derived metallic melt
CMB topography and lateral velocity gradients of vϕ during a cycle of
Origins of ultralow velocity zones through slab-derived metallic melt
Slab control on the mega-sized North Pacific ultra-low velocity zone
Structure, Materials and Processes in the Earth's Core and Mantle
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Recurrence time and size of Chilean earthquakes influenced by geological structure,Nature Geoscience - X-MOL
Subducted oceanic crust as the origin of seismically slow lower-mantle structures, Progress in Earth and Planetary Science
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