Video Experimental Relacionado

Updated: Jun 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

El derretimiento de la peridotita a 140 gigapascals

G Fiquet1, A L Auzende, J Siebert

  • 1Institut de Minéralogie et de Physique des Milieux Condensés, Institut de Physique du Globe de Paris, Université Pierre et Marie Curie, UMR CNRS 7590, Université Paris Diderot, 140 rue de Lourmel, 75015 Paris, France. guillame.fiquet@impmc.upmc.fr

Science (New York, N.Y.)
|September 18, 2010
PubMed
Resumen

La fusión parcial puede ocurrir en el manto más bajo de la Tierra, lo que explica las velocidades sísmicas ultrabajas. Los experimentos confirman la fusión en las condiciones del límite entre el núcleo y el manto, lo que sugiere que las regiones fundidas albergan elementos incompatibles.

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