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Science 24 January 2003:
Vol. 299. no. 5606, pp. 552 - 555
DOI: 10.1126/science.1078159

Reports

Robust Normal Mode Constraints on Inner-Core Anisotropy from Model Space Search

Caroline Beghein,* Jeannot Trampert

A technique for searching full model space that was applied to measurements of anomalously split normal modes showed a robust pattern of P-wave and S-wave anisotropy in the inner core. The parameter describing P-wave anisotropy changes sign around a radius of 400 kilometers, whereas S-wave anisotropy is small in the upper two-thirds of the inner core and becomes negative at greater depths. Our results agree with observed travel-time anomalies of rays traveling at epicentral distances varying from 150° to 180°. The models may be explained by progressively tilted hexagonal close-packed iron in the upper half of the inner core and could suggest a different iron phase in the center.

Faculty of Earth Sciences, Utrecht University, Post Office Box 80021, 3508 TA Utrecht, Netherlands.
*   To whom correspondence should be addressed. E-mail: beghein{at}geo.uu.nl


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THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Elastic Anisotropy of Earth's Inner Core.
A. B. Belonoshko, N. V. Skorodumova, A. Rosengren, and B. Johansson (2008)
Science 319, 797-800
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Science. ISSN 0036-8075 (print), 1095-9203 (online)