Hetzel, R.: Geology of the Bozdag area, central Menderes massif, sw Turkey : Pan-african basement and alpine deformation
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Personen: Hetzel, R. (Autor) 
Romer, R. L. (Autor) 
Candan, O. (Autor) 
Passchier, Cornelis Willem (Autor) 
  
Titel: Geology of the Bozdag area, central Menderes massif, sw Turkey : Pan-african basement and alpine deformation
  
Quelle: Geologische Rundschau. Bd. 87. H. 3. Berlin : Springer. S. 394 - 406
Erscheinungsjahr:    1998
ISBN / ISSN: 0016-7835
URL der Originalveröffentlichung doi:10.1007/s005310050218
  
Dokumentart:
Zeitschriftenaufsatz Zeitschriftenaufsatz
Sprache: Englisch
Open Access:
Person der Universität:    Passchier, Cornelis Willem  In UnivIS suchen 
Einrichtung: Institut für Geowissenschaften
DDC-Sachgruppe:    Geowissenschaften
ID: 52624  Universitätsbibliothek Mainz
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Informationen zu den Nutzungsrechten unserer Inhalte Informationen zu den Nutzungsrechten unserer Inhalte
Abstract: The Menderes massif consists of a Precambrian Core Series that preserves evidence for a polymetamorphic history and a Paleozoic/Mesozoic Cover Series that experienced only the Alpine tectonometamorphic evolution. Structural, petrographic, and geochronologic investigations in the central Menderes massif demonstrate that (a) part of the metamorphic and structural evolution of the Precambrian basement is older than the undeformed 551+/-1.4-Ma-old Birgi metagranite, and (b) inferred Alpine fabrics overprinting the Cover Series largely have the same attitudes as the old structures in the much older Core Series. The inferred Alpine fabrics include both contractional and extensional structures. Contraction under greenschist to amphibolite facies conditions resulted in the imbrication of the Core and Cover Series and generated an inverted metamorphic sequence by north-directed thrusting. During Alpine extension, most of the south-dipping thrust faults were reactivated as extensional shear zones under decreasing greenschist facies conditions.
   
  
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