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Updated: Jun 8, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
06:04

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Published on: November 15, 2013

La estructura del hierro en el núcleo interno de la Tierra

Shigehiko Tateno1, Kei Hirose, Yasuo Ohishi

  • 1Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Ookayama, Meguro, Tokyo 152-8551, Japan. tateno.s.aa@m.titech.ac.jp

Science (New York, N.Y.)
|October 16, 2010
PubMed
Resumen

El núcleo interno de la Tierra es principalmente de hierro (Fe). Los experimentos muestran que el hierro hexagonal compacto (hcp) es estable en condiciones del núcleo interno, lo que sugiere que su estructura explica la anisotropía sísmica.

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