2026-06-26T21:18:42Zhttps://docta.ucm.es/rest/oai/request

oai:docta.ucm.es:20.500.14352/651902024-07-24T17:29:49Zcom_20.500.14352_14col_20.500.14352_15

Navidad Fernández De La Cruz, Marina Peinado, Mercedes 2023-06-21T02:15:21Z 2023-06-21T02:15:21Z 1981 0378-102X https://hdl.handle.net/20.500.14352/65190 https://revistas.ucm.es/index.php/CGIB/issue/view/CGIB818111 This paper deals with an augengneis unit called Antonita-gneis. On the basis of their petrological and geochemical characteristies these gneisses are considered as old 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. spa open access Ortogneises y metasedimentos de la formación infrabasal al Ollo de Sapo (Macizo de Hiendelaencina, Guadarrama Oriental) journal article