Origin of ULVZs near the African LLSVP: Implications from their distribution and characteristics
An Fan, Xinlei Sun
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The core-mantle boundary region under the Gulf of Alaska : no ULVZ for shear waves
The Earth's core-mantle boundary (CMB) marks the boundary between the hot, molten iron core and the silicate mantle and is a thermal, chemical, and flow boundary. Previous observations of very slow compressional wavespeeds suggest that thin ultra-low-velocity zones (ULVZs), possibly composed of a mixture of molten iron and silicates, exist at the base ...
Castle, John C., Hilst, R.D. van der
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Tracking the origin of ultralow velocity zones at the base of Earth's mantle. [PDF]
Chen J.
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The evolution of the Galápagos mantle plume. [PDF]
Soderman CR +5 more
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Seismic noise, particularly the microseism generated by the oceans, is a fundamental limitation on using short period (1 - 10 s) teleseismic data to study the deep Earth. Deep learning auto-encoders have proven effective at denoising seismic data in other applications.
Stuart Russell +5 more
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Melting and defect transitions in FeO up to pressures of Earth's core-mantle boundary. [PDF]
Dobrosavljevic VV +8 more
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Mineralogy of the deep lower mantle in the presence of H2O. [PDF]
Hu Q +7 more
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Cascadia low frequency earthquakes at the base of an overpressured subduction shear zone. [PDF]
Calvert AJ +3 more
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Xenon iron oxides predicted as potential Xe hosts in Earth's lower mantle. [PDF]
Peng F +6 more
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Structural dynamics of basaltic melt at mantle conditions with implications for magma oceans and superplumes. [PDF]
Majumdar A +4 more
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