A low attenuation layer in the Earth's uppermost inner core
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/195/3/2005/17052859/ggt368.pdf
Reference49 articles.
1. Melting-induced stratification above the Earth's inner core due to convective translation;Alboussière;Nature,2010
2. Thermochemical flows couple the Earth's inner core growth to mantle heterogeneity;Aubert;Nature,2008
3. Solidification of the Earth's core;Bergman,2003
4. Elastic and attenuation anisotropy in directionally solidified (hcp) zinc, and the seismic anisotropy in the Earth's inner core;Bergman;Phys. Earth. planet. Inter.,2000
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1. Small-scale heterogeneities at the bottom of the lower mantle beneath the northern Bay of Bengal and the northern Gulf of Mexico by the analysis of PKP precursors;Geophysical Journal International;2023-11-08
2. A Search for Large‐Scale Variations in the Fine‐Scale Structure of Earth's Inner Core;Journal of Geophysical Research: Solid Earth;2022-09
3. An attenuating, isotropic and heterogeneous uppermost inner core: evidence from global PKiKP-PKIKP amplitude ratio tomography;Geophysical Journal International;2022-04-11
4. Seismic tomography of the uppermost inner core;Earth and Planetary Science Letters;2019-12
5. Variations of Velocity and Attenuation Anisotropy Structures in the Uppermost Inner Core Beneath the Central Pacific Region;Geophysical Research Letters;2019-11-06
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