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...

Olles dieđut

Bibliográfalaš dieđut
Váldodahkki: Wood, B
Materiálatiipa: Journal article
Giella:English
Almmustuhtton: 1995

Geahča maid