Video Experimental Relacionado

Updated: Jul 18, 2026

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

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Published on: November 15, 2013

Estabilidad del derretimiento hidroso en la base del manto superior de la Tierra

Tatsuya Sakamaki1, Akio Suzuki, Eiji Ohtani

  • 1Department of Earth and Planetary Material Sciences, Tohoku University, Sendai 980-8578, Japan.

Nature
|January 13, 2006
PubMed
Resumen

El magma hidroso puede ser estable por encima de la discontinuidad de 410 km. Este hallazgo apoya la presencia de fusión en zonas de baja velocidad dentro del manto superior de la Tierra, lo que explica las anomalías sísmicas.

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