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

Hasozbek, Altug; AKAY, ERHAN; Erdogan, Burhan; Satir, Muharrem; Siebel, Wolfgang

doi:10.1016/j.jog.2010.03.002

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, Scopus)

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
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.