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Basalt-eclogite transition

The basalt - gabbro (the amphibole - in the case of water presence) transition to eclogite happens in upper mantle at the continental condition. [Pg.731]

Figure 6. Penetration of water down to Mohorovichich boundary (1) prevents phase transition "eclogite - basalt" (2) according to the geoterm 3 in the Standard Earth Crust. Pressure is given in GPa. Granate -granulite is shown (4). Figure 6. Penetration of water down to Mohorovichich boundary (1) prevents phase transition "eclogite - basalt" (2) according to the geoterm 3 in the Standard Earth Crust. Pressure is given in GPa. Granate -granulite is shown (4).
See other pages where Basalt-eclogite transition is mentioned: [Pg.23]    [Pg.749]    [Pg.749]    [Pg.750]    [Pg.756]    [Pg.45]    [Pg.45]    [Pg.46]    [Pg.52]    [Pg.731]    [Pg.65]   
See also in sourсe #XX -- [ Pg.23 ]



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Basalt

Eclogite

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