M Li - Mantle convection and surface expressions, 2021 - Wiley Online Library
The oceanic crust is created at mid‐ocean ridges and returned to the Earth's deep mantle at subduction zones. A clear picture on the dynamics and distribution of the subducted oceanic …
The abrupt changes in mineralogical properties across the Earth's mantle transition zone substantially impact convection and thermochemical fluxes between the upper and lower …
Seismology records the presence of various heterogeneities throughout the lower mantle,, but the origins of these signals—whether thermal or chemical—remain uncertain, and …
A viscosity jump of one to two orders of magnitude in the lower mantle of Earth at 800–1,200- km depth is inferred from geoid inversions and slab-subducting speeds. This jump is known …
A better understanding of the Earth's compositional structure is needed to place the geochemical record of surface rocks into the context of Earth accretion and evolution …
The Hawaiian-Emperor seamount chain that includes the Hawaiian volcanoes was created by the Hawaiian mantle plume. Although the mantle plume hypothesis predicts an oceanic …
Seismic discontinuities in the mantle are indicators of its thermo-chemical state and offer clues to its dynamics. Ray-based seismic methods, though limited by the approximations …
The nature of compositional heterogeneity in Earth's lower mantle remains a long-standing puzzle that can inform about the long-term thermochemical evolution and dynamics of our …
The mantle transition zone (MTZ) of Earth is demarcated by solid‐to‐solid phase changes of the mineral olivine that produce seismic discontinuities at 410 and 660‐km depths. Mineral …