Mantle plumes originate at depths near the core− mantle boundary (~ 2,800 km). As such, they provide invaluable information about the composition of the deep mantle and insight …
Plate tectonics shapes Earth's surface, and is linked to motions within its deep interior,. Cold oceanic lithosphere sinks into the mantle, and hot mantle plumes rise from the deep Earth …
Understanding the long-term evolution of Earth's plate–mantle system is reliant on absolute plate motion models in a mantle reference frame, but such models are both difficult to …
High-temperature isotope fractionation during partial melting and other igneous differentiation processes has been observed in many non-traditional isotope systems. The …
Convective flow in the deep mantle controls Earth's dynamic evolution, influences plate tectonics, and has shaped Earth's current surface features. Present and past convection …
DA Frost, M Lasbleis, B Chandler, B Romanowicz - Nature Geoscience, 2021 - nature.com
Progressive crystallization of Earth's inner core drives convection in the outer core and magnetic field generation. Determining the rate and pattern of inner-core growth is thus …
S Kim, H Tkalčić, J Rhie - Journal of Geophysical Research …, 2017 - Wiley Online Library
The magmatic process of continental intraplate volcanism (CIV) is difficult to understand due to heterogeneous interactions with the crust and the lithospheric upper mantle. Mount …
J Stephenson, H Tkalčić… - Journal of Geophysical …, 2021 - Wiley Online Library
The model of cylindrical anisotropy in the inner core (IC) states that seismic rays traveling parallel to the Earth's rotational axis travel faster than those parallel to the equator. There …
S Burdick, V Lekić - Geophysical Journal International, 2017 - academic.oup.com
High-resolution models of seismic velocity variations constructed using body-wave tomography inform the study of the origin, fate and thermochemical state of mantle domains …