Early Miocene granite formation by detachment tectonics or not? A case study from the northern Menderes Massif (Western Turkey)
JOURNAL OF GEODYNAMICS, vol.50, no.2, pp.67-80, 2010 (SCI-Expanded, Scopus)
- Publication Type: Article / Article
- Volume: 50 Issue: 2
- Publication Date: 2010
- Doi Number: 10.1016/j.jog.2010.03.002
- Journal Name: JOURNAL OF GEODYNAMICS
- Journal Indexes: Science Citation Index Expanded (SCI-EXPANDED), Scopus
- Page Numbers: pp.67-80
- Keywords: Egrigoz granite, Koyunoba granite, Geochronology, Menderes Massif, Geochemistry
- Dokuz Eylül University Affiliated: Yes
Abstract
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.