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    STUDIA GEOLOGIA - Issue no. 3 / 2003  
         
  Article:   PETROLOGY OF GARNET-AMPHIBOLITE WITH WHITE MICA FROM VRANJSKA BANJA SERIES (SERBIAN-MACEDONIAN MASSIF, SE SERBIA).

Authors:  NADA VASKOVIC, VESNA MATOVIC, DANICA SRECKOVIC-BATOCANIN.
 
       
         
  Abstract:  The Upper Complex of the Serbian-Macedonian Massif (SMM) named also Vlasina Complex – (VC) is mostly composed of greenschist with subordinate medium to high grade metamorphics (Dimitrijevic, 1959; Petrovic, 1965). This Ripheo-Cambrian complex was firstly intruded by Ordovician granitoids, later by Paleogene Surdulica granitoid and underwent the extensive Oligocene-Miocene volcanic activity. According to the spatial position, lithology and metamorphic features, the VC was divided into six series as follows: Vlasina (Vaskovic & Tasic, 2000), Vranjska Banja, Bozica, Lisina, Jaresnik and Stajevac (Babovic et al., 1977). ...  
         
     
         
         
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