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Anisotropy of the inner core inferred from PKIKP travel times

Morelli, Andrea, Dziewonski, Adam M., Woodhouse, John H.·1986·Geophysical Research Letters

Abstract

Travel‐time residuals of the PKIKP phase observed between 170° and 180° show an axisymmetric pattern of degree 2 with an amplitude of about 2 seconds. The effect at shorter distances is much less pronounced and the entire data set cannot be explained by a physically realistic radial distribution of (isotropic) heterogeneity. We propose that, in addition to the general (isotropic) heterogeneity, the inner core is anisotropic with cylindrical symmetry aligned with the earth's rotation axis. Average P‐velocity along this axis is about 1 percent faster than in the equatorial plane.

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Metadata

Authors
Morelli, A., Dziewonski, A. M., & Woodhouse, J. H.
Venue
Geophysical Research Letters
Published
1986-12
Volume
13
Issue
13
Pages
1545-1548
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W2070798574
Cited by
414
References
0
FWCI
5.90
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Anisotropy of the inner core inferred from PKIKP travel times. https://app.cochat.ai/papers/10.1029/gl013i013p01545
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Morelli, A., Dziewonski, A. M., & Woodhouse, J. H. (1986). Anisotropy of the inner core inferred from PKIKP travel times. Geophysical Research Letters. https://doi.org/10.1029/gl013i013p01545

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