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Garnets orogenic peridotite massifs

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 Garnets orogenic peridotite massifs is mentioned: [Pg.807] [Pg.809] [Pg.105] [Pg.107] [Pg.806] [Pg.807] [Pg.807] [Pg.810] [Pg.811] [Pg.812] [Pg.813] [Pg.847] [Pg.849] [Pg.850] [Pg.1074] [Pg.104] [Pg.105] [Pg.105] [Pg.108] [Pg.109] [Pg.110] [Pg.111] [Pg.145] [Pg.147] [Pg.148] [Pg.374] [Pg.841] [Pg.139]

See also in sourсe #XX -- [ Pg.145 , Pg.149 ]

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Garnet

Garnets garnet

Orogenic peridotite massifs

Orogenic peridotite massifs garnet peridotites

Orogenic peridotite massifs peridotites

Peridotites