Video Experimental Relacionado

Updated: Jul 9, 2026

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

Simulation of the Planetary Interior Differentiation Processes in the Laboratory

Published on: November 15, 2013

Interdifusión Fe-Mg en (Mg,Fe) SiO3 Perovskita y reequilibrio del manto inferior para el reequilibrio

Christian Holzapfel1, David C Rubie, Daniel J Frost

  • 1Bayerisches Geoinstitut, University of Bayreuth, D-95440 Bayreuth, Germany. c.holzapfel@mx.uni-saarland.de

Science (New York, N.Y.)
|July 30, 2005
PubMed
Resumen

La difusión de hierro y magnesio en la perovskita es extremadamente lenta, lo que limita la homogeneización química en el manto inferior de la Tierra. Esto sugiere que las heterogeneidades persisten a menos que se produzca una deformación intensa.

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