Anisotropy at the Inner Core Boundary
Author:
Affiliation:
1. Earth‐Life Science Institute Tokyo Institute of Technology Tokyo Japan
2. Géosciences Montpellier UMR CNRS 5243, Université Montpellier 2 Montpellier France
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL083644
Reference42 articles.
1. Melting-induced stratification above the Earth’s inner core due to convective translation
2. Irregular Transition Layer Beneath the Earth's Inner Core Boundary From Observations of Antipodal PKIKP and PKIIKP Waves
3. 3-D seismic velocities calculated from lattice-preferred orientation and reflectivity of a lower crustal section: examples of the Val Sesia section (Ivrea zone, northern Italy)
4. Short wavelength topography on the inner-core boundary
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2. An attenuating, isotropic and heterogeneous uppermost inner core: evidence from global PKiKP-PKIKP amplitude ratio tomography;Geophysical Journal International;2022-04-11
3. Antipodal seismic reflections upon shear wave velocity structures within Earth's inner core;Physics of the Earth and Planetary Interiors;2021-12
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