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Updated: Dec 27, 2025

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Volcanismo intraplate originado en la zona de transición del manto hidroso ascendente

Jianfeng Yang1, Manuele Faccenda2

  • 1Dipartimento di Geoscienze, Università di Padova, Padova, Italy.

Nature
|February 28, 2020
PubMed
Resumen

El vulcanismo intraplate y petit-spot, anteriormente inexplicable, está relacionado con la subducción de losas del Pacífico que interactúan con una zona de transición del manto hidroso. Esta interacción libera agua, creando zonas de manto de baja velocidad e impulsando el volcanismo.

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