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The late Oligocene evolution of the southern Menderes Massif in western Turkey consists of deformation in the crustal-scale, moderately dipping, ductile shear zone. From the southern flank from the Menderes Massif, western Turkey, an E–W-trending quartz–mica vein was regarded within the augen gneisses on the so-called ‘Main’ collection. Вместе с http://lkocaklar05936.atualblog.com/6983743/için-basit-anahtar-bozkurtlar-geliyor-örtüsünü


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