Faculty Publications
Document Type
Article
Abstract
Seismic anisotropy in the Earth’s inner core refers to the observation that seismic waves travel faster along the Earth’s rotation axis than in the equatorial plane, a feature inferred from decades of global seismological observations. This directional dependence of wave speeds provides important clues about the structure, composition and dynamics of the inner core. Here we explore a coupled thermo-mechanical mechanism for the generation of inner core anisotropy, focusing on the effects of anisotropic thermal conductivity in iron crystals as the inner core cools. We propose that the higher thermal conductivity of iron along the crystallographic c-axis compared with the a-axis leads to differential heat flow, generating temperature anomalies within the inner core. These anomalies drive flow and contribute to the development of elastic anisotropy. Our model suggests that this thermally induced flow mechanism can account for the observed seismic anisotropy without requiring extrinsic contributions. These findings provide insights into the internal dynamics of the inner core, providing a more comprehensive understanding of its thermal evolution and anisotropic properties.
Digital Object Identifier (DOI)
Publication Info
Published in Nature Geoscience, Volume 19, 2026.
Rights
This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.
APA Citation
Das, P. P., Buffett, B., & Frost, D. (2026). Generation of inner core anisotropy by anisotropic thermal conductivity of iron crystals. Nature Geoscience, 19, 353–358. https://doi.org/10.1038/s41561-026-01916-3