Video Experimental Relacionado

Updated: Apr 29, 2026

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
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Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions

Published on: June 13, 2015

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Lentes de magma congelado debajo de la corteza oceánica

Mladen R Nedimović1, Suzanne M Carbotte, Alistair J Harding

  • 1Lamont-Doherty Earth Observatory of Columbia University, 61 Route 9W, PO Box 1000, Palisades, New York 10964-8000, USA. mladen@ldeo.columbia.edu

Nature
|August 27, 2005
PubMed
Resumen

Los datos sísmicos revelan lentes de gabbro y acumulaciones de fundido en la zona de transición de Moho, lo que sugiere que la corteza oceánica se forma a partir de múltiples cuerpos de magma, no solo uno. Este hallazgo apoya un nuevo modelo para la generación de corteza en las cordilleras oceánicas medias.

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