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Updated: Feb 24, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
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Un espesor continental unificado de la sismología y los diamantes sugiere una placa definida por el derretimiento

Saikiran Tharimena1, Catherine Rychert2, Nicholas Harmon2

  • 1Ocean and Earth Science, National Oceanography Centre, University of Southampton, Southampton SO14 3ZH, UK. s.tharimena@noc.soton.ac.uk.

Science (New York, N.Y.)
|August 12, 2017
PubMed
Resumen

Las placas continentales tienen un límite distinto de alrededor de 130-190 km de profundidad, probablemente definido por el derretimiento parcial. Este hallazgo concilia los datos geoquímicos y sísmicos sobre el grosor de la litosfera.

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