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Updated: May 5, 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

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La anisotropía paralela a la zanja producida por la deformación serpentina en la cuña hidratada del manto hidratado

Ikuo Katayama1, Ken-ichi Hirauchi, Katsuyoshi Michibayashi

  • 1Department of Earth and Planetary Systems Science, Hiroshima University, Higashi-Hiroshima 739-8526, Japan. katayama@hiroshima-u.ac.jp

Nature
|October 23, 2009
PubMed
Resumen

La serpentina, un mineral hidratado, puede explicar la fuerte anisotropía sísmica paralela a las trincheras en las zonas de subducción. Su orientación cristalina durante la deformación crea variaciones significativas de la velocidad sísmica, a diferencia del olivino solo.

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