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Geoquímica del granito de dos micas de A Espenuca: origen y evolución
(Universidade da Coruña, 1994)
[Abstract] The A Espenuca two-mica granite, situated in the northern sector ofthe Central Iberian Zone, was variably deformed by the Valdoviño Fault. Deformation intensity is observed to increase from W to E, also being ...