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handle: 10261/6019 , 20.500.14352/65190
This paper deals with an augengneis unit called Antonita-gneis. On the basis of their petrological and geochemical characteristies these gneisses are considered as oíd two-mica granites, with a silicosodic trend. These gneisses and their late manifestations (metaaplites and metapegmatites) are induded in a metasedimentary series, belonging to the metamorphic grade of staurolite - kyanite.
Peer reviewed
Metasedimentos, Formación Ollo de Sapo, Ortogneises, Ortogénesis, Sistema Central, Petrología, 552(234.1), Sistema Central español
Metasedimentos, Formación Ollo de Sapo, Ortogneises, Ortogénesis, Sistema Central, Petrología, 552(234.1), Sistema Central español
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