Video Experimental Relacionado

Updated: Aug 8, 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

Dependencia multivariable de la partición Fe-Mg en el manto inferior

Mao1, Shen, Hemley

  • 1Geophysical Laboratory and Center for High Pressure Research, Carnegie Institution of Washington, 5251 Broad Branch Road, NW, Washington, DC 20015-1305 USA.

Science (New York, N.Y.)
|January 4, 1998
PubMed
Resumen

La partición del hierro y el magnesio en el manto inferior de la Tierra depende de la presión y la temperatura. El hierro férrico afecta la composición de la perovskita, influyendo en las propiedades profundas de la Tierra.

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