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    STUDIA GEOLOGIA - Issue no. Special%20Issue / 2009  
         
  Article:   METAMORPHIC CONDITIONS OF THE REBRA GROUP IN THE MARAMUREŞ MOUNTAINS, NORTH ROMANIA.

Authors:  EMILIA MOSONYI, FORRAY FERENC LÁZÁR. 		 
       
         
  Abstract:  In the southern part of the Maramureş Mountains (Eastern Carpathians, north Romania) the three Alpine units of the Median Dacides (MD), i.e. the Bucovinian, Sub-Bucovinian and Infrabucovinian nappes, respectively are cropping out. Each MD nappe consists of prealpine metamorphics and Palaeozoic-Mesozoic sediments. The pre-Alpine rocks are assigned to several metamorphic complexes i.e. the Rebra, Negrişoara, Tulgheş, and Bretila (Săndulescu, 1984), separated in between by predominantly Variscan, rarely Alpine mylonitic shear zones.

Keywords: Eastern Carpathians, Median Dacides, Alpine nappe system, tectonic window, mylonitic zones, tourmaline-biotite geothermometry, phengite geobarometry
  
         
     
         
         
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