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    STUDIA GEOLOGIA - Issue no. 2 / 2002  
         
  Article:   NEW LITHOSTRATIGRAPHIC AND STRUCTURAL ASPECTS IN THE SOUTHERN PART OF THE BIHOR MASSIF (APUSENI MOUNTAINS).

Authors:  IOAN CORIOLAN BALINTONI, ADRIAN PUŞTE.
 
       
         
  Abstract:  The Muncel Series (Ionescu, 1962), from the Bihor massif can be included in the Permian Păiuşeni Lithogroup, because it consists predominantly from weak metamorphosed granites and porphyres. In this idea, the Highiş Nappe correlates with the Muncel Nappe and does not with the Poiana Nappe. Consequently, the down to up succession of the Biharia Nappe System becomes: the Grda Nappe; The Raviceşti scale; the Poiana Nappe; the Piatra Grăitoare scale; the Biharia nappe; the Highiş-Muncel Nappe; the Baia de Arieş Nappe.  
         
     
         
         
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