Some dynamical consequences of partial melting in Earth’s deep mantle, Phys. Earth planet
We use regional scale numerical models of mantle convection to investigate the simple hypothesis that seismically anomalous thin patches of Earth's lowermost mantle, termed "ultralow-velocity zones" or ULVZ, are derived from partial ...
John W Hernlund, Paul J Tackley
core
Spin transition in magnesiowüstite and ultralow thermal conduction in ultralow velocity zones. [PDF]
Hsieh WP +6 more
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Efficient hybrid numerical modeling of the seismic wavefield in the presence of solid-fluid boundaries. [PDF]
Lyu C, Romanowicz B, Zhao L, Masson Y.
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Deep mantle anomalies block early Earth melting, challenging a primordial origin. [PDF]
Roy A, Mittelstaedt E, Cooper CM.
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Compositionally-distinct ultra-low velocity zones on Earth's core-mantle boundary. [PDF]
Li M, McNamara AK, Garnero EJ, Yu S.
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Dynamics of longitudinal Hawaiian hotspot motion and the formation of the Hawaiian-Emperor Bend. [PDF]
Zhang J, Hu J.
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Extensive iron-water exchange at Earth's core-mantle boundary can explain seismic anomalies. [PDF]
Kawano K +5 more
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Thermodynamics of the lowermost mantle
Seismic observations of the region above the core mantle boundary (CMB), including Ultra-Low Velocity Zones (ULVZ) and D” discontinuities, and recent mineral physics data suggest the bottom of the mantle may be chemically heterogeneous, possibly, on ...
Sun, D., Ahrens, T. J., Asimow, P. D.
core
Origins of ultralow velocity zones through slab-derived metallic melt. [PDF]
Liu J, Li J, Hrubiak R, Smith JS.
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Ancient storage of anomalous mercury isotope signatures in the Earth's transition zone. [PDF]
Xu R +15 more
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