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Evidencia sísmica para el transporte de aguas profundas en el manto

Hitoshi Kawakatsu1, Shingo Watada

  • 1Earthquake Research Institute, University of Tokyo, 1-1-1 Yayoi, Bunkyo-ku, Tokyo 113-0032, Japan. hitosi@eri.u-tokyo.ac.jp

Science (New York, N.Y.)
|June 9, 2007
PubMed
Resumen

Los datos sísmicos revelan cómo el agua viaja profundamente en el manto de la Tierra a través de la zona de subducción de Japón. El agua escapa de la corteza oceánica hidratada, formando un canal del manto que la transporta al manto profundo.

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