The Effect of H2O on the 410-Kilometer Seismic Discontinuity.

The Effect of H2O on the 410-Kilometer Seismic Discontinuity.

The 410-kilometer seismic discontinuity is generally considered to be caused by a phase transformation of the main constituent of the upper mantle, olivine, alpha-(Mg,Fe)(2)SiO(4), to beta-(Mg,Fe)(2)SiO(4). Recent data show that H(2)O dissolves in olivine and other nominally anhydrous mantle mineral...

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Dades bibliogràfiques
Autor principal:	Wood, B
Format:	Journal article
Idioma:	English
Publicat:	1995

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