Video Experimental Relacionado

Updated: Jul 26, 2026

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
11:50

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

Published on: June 13, 2015

El grosor de la corteza fuera del eje a través y a lo largo de la elevación del Pacífico Este dentro del área MELT

Canales1, Detrick, Bazin

  • 1J. P. Canales and R. S. Detrick, Department of Geology and Geophysics, Woods Hole Oceanographic Institution, 360 Woods Hole Road, Woods Hole, MA 02543, USA. S. Bazin, A. J. Harding, J. A. Orcutt, Institute of Geophysics and Planetary.

Science (New York, N.Y.)
|June 5, 1998
PubMed
Resumen

Las placas de Nazca y del Pacífico exhiben un grosor de corteza similar, que difiere de las variaciones de profundidad y gravedad a través de la subida del Pacífico Este. Estas diferencias probablemente se derivan de las variaciones de densidad del manto, no de la edad de la corteza.

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