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Orogenic peridotite massifs garnet peridotites

The intermediate pressure (IP) orogenic peridotites include several massifs dominantly equilibrated in the spinel ( amphibole, phlogopite) peridotite facies, either in the Ariegite (garnet in mafic layers) or in the Seiland (mafic layers devoid of garnet) subfacies (O Hara, 1967a Obata, 1980). These massifs were generally... [Pg.811]

See other pages where Orogenic peridotite massifs garnet peridotites is mentioned: [Pg.807]    [Pg.809]    [Pg.105]    [Pg.107]    [Pg.806]    [Pg.807]    [Pg.807]    [Pg.810]    [Pg.811]    [Pg.812]    [Pg.841]    [Pg.847]    [Pg.849]    [Pg.850]    [Pg.1074]    [Pg.104]    [Pg.105]    [Pg.105]    [Pg.108]    [Pg.109]    [Pg.110]    [Pg.139]    [Pg.145]    [Pg.147]    [Pg.148]    [Pg.374]    [Pg.813]    [Pg.111]   
See also in sourсe #XX -- [ Pg.108 ]



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