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Updated: Jul 12, 2026

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

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Published on: November 15, 2013

La partición del hierro en el manto de la Tierra: hacia una discontinuidad profunda del manto inferior

James Badro1, Guillaume Fiquet, François Guyot

  • 1Laboratoire de Mine Université ralogie-Cristallographie de Paris, Université Paris VI, Université Paris 7, CNRS, IPGP, 4 place Jussieu, F-75252 Paris Cedex 05, France.

Science (New York, N.Y.)
|April 5, 2003
PubMed
Resumen

El hierro en el manto inferior de la Tierra sufre una transición de alta espina a baja espina alrededor de 2000 km de profundidad. Esto hace que el hierro se concentre en ferropericlase, creando potencialmente capas distintas en el manto profundo.

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