Published January 1, 2010
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Early Miocene granite formation by detachment tectonics or not? A case study from the northern Menderes Massif (Western Turkey)
- 1. Dokuz Eylul Univ, Fac Engn, Dept Geol Engn, TR-35160 Izmir, Turkey
- 2. Univ Tubingen, Inst Geowissensch, D-72074 Tubingen, Germany
Description
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.
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