Early Miocene granite formation by detachment tectonics or not? A case study from the northern Menderes Massif (Western Turkey)

Hasozbek A., AKAY E., Erdogan B., Satir M., Siebel W.

JOURNAL OF GEODYNAMICS, cilt.50, sa.2, ss.67-80, 2010 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 50 Sayı: 2
  • Basım Tarihi: 2010
  • Doi Numarası: 10.1016/j.jog.2010.03.002
  • Dergi Adı: JOURNAL OF GEODYNAMICS
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.67-80
  • Anahtar Kelimeler: Egrigoz granite, Koyunoba granite, Geochronology, Menderes Massif, Geochemistry, METAMORPHIC CORE COMPLEX, NORTHWESTERN ANATOLIA, ZIRCON AGES, SW TURKEY, EXHUMATION HISTORY, MAGMATIC ACTIVITY, AUGEN GNEISSES, EVOLUTION, GEOCHRONOLOGY, DEFORMATION
  • Dokuz Eylül Üniversitesi Adresli: Evet

Özet

The northern border of the Menderes Massif is dominated by gneiss-schist-marble association and meta-granites. The high-grade units of the massif are tectonically overlain by a meta-platform sequence of the Afyon Zone and the Cretaceous-early Tertiary HP/LT Tavsanli Zone. The Simav Magmatic Complex, comprising the shallow-seated, I-type, calc-alkaline, post-collisional Egrigoz and Koyunoba granites, and associated subvolcanic-volcanic sequences crosscuts the Menderes Massif, Afyon Zone and tectonic contact between them.