Results 51 to 60 of about 121 (99)

The core-mantle boundary region under the Gulf of Alaska : no ULVZ for shear waves

open access: yes, 2000
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
openaire   +1 more source

The evolution of the Galápagos mantle plume. [PDF]

open access: yesSci Adv, 2023
Soderman CR   +5 more
europepmc   +1 more source

Denoising teleseismic data for deep Earth studies using a supervised deep-learning auto-encoder: a case study of diffracted waves from ULVZs

open access: yes
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
openaire   +1 more source

Melting and defect transitions in FeO up to pressures of Earth's core-mantle boundary. [PDF]

open access: yesNat Commun, 2023
Dobrosavljevic VV   +8 more
europepmc   +1 more source

Mineralogy of the deep lower mantle in the presence of H2O. [PDF]

open access: yesNatl Sci Rev, 2021
Hu Q   +7 more
europepmc   +1 more source

Xenon iron oxides predicted as potential Xe hosts in Earth's lower mantle. [PDF]

open access: yesNat Commun, 2020
Peng F   +6 more
europepmc   +1 more source

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