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Updated: May 15, 2026

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

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Published on: November 15, 2013

La evidencia de níquel y helio para la fusión por encima del límite núcleo-manto

Claude Herzberg1, Paul D Asimow, Dmitri A Ionov

  • 1Department of Earth and Planetary Sciences, Rutgers University, 610 Taylor Road, Piscataway, New Jersey 08854-8066, USA. herzberg@rci.rutgers.edu

Nature
|January 11, 2013
PubMed
Resumen

Las altas proporciones de helio-3 a helio-4 en los basaltos sugieren un origen de una fuente profunda de la Tierra. Esta fuente de manto rica en níquel y menos desgasificada probablemente se formó temprano en la historia de la Tierra a través de interacciones núcleo-manto.

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