By Klaus Gessner, Uwe Ring, Talip Güngör
This field-trip advisor explores the tectonics of Samos and the Menderes Massif, interesting parts in the jap Mediterranean element of the Tethyan orogen. The consultant comprises specified outcrop descriptions, maps, and diagrams to discover along-strike adaptations within the Hellenide-Anatolide orogen, together with the structure of the Early Tertiary Alpine nappe stack and its powerful Miocene extensional overprint. The steered itinerary relies at the 2010 Geological Society of the USA box discussion board: "Significance of Along-Strike adaptations for the three-D structure of Orogens: The Hellenides and Anatolides within the jap Mediterranean." The outcrop descriptions start with Day 1 in Samos, the place, atypically for the N-S-stretched Aegean zone, Miocene extension is E-W. the point of interest of Day 2 is on high-pressure assemblages in northern Samos. the next 3 days discover the Anatolide Belt in western Turkey, the place the Menderes nappes-also referred to as the Menderes Massif-form the tectonic footwall less than the Cycladic Blueschist Unit.
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Extra resources for Field Guide to Samos and the Menderes Massif: Along-Strike Variations in the Mediterranean Tethyan Orogen (GSA Field Guide 23)
Park the car in the village and walk north along a valley for ~900 m until you see the outcrop on your right (Fig. 51). Field Guide to Samos and the Menderes Massif 41 A Figure 45. Map of localities in the western Aydın Mountains. Inset A shows location of Figure 46. Modified from © 2011 Google—Map data © 2011 Basarsoft, Tele Atlas. 1 Figure 46. Map of the Ballikkayası Tepe and Bozkaya Tepesi area. Modified from © 2011 Google—Map data © 2011 Basarsoft, Tele Atlas. 0 ive lower boun dary o f p en etr at 10 00 S A3 o A’′ A 44 Bozkaya T.
Location. 60″ E) (Fig. 43). Access. Drive from Beydağ SE on the Nazilli road (35-33), climbing into the Aydın Mountains. The outcrop is between Beydağ and Çamlık, ~500 m after the first hairpin corner after leaving Beydağ. Geology. Both foliated and undeformed granitic rocks of the Çine Nappe are exposed. Shear bands in protomylonites indicate a north-directed sense of shear. Foliation in this area generally dips NW. 11. Metabasic Lenses in Çine Nappe Summary. Metabasic asymmetric boudins in Çine Nappe gneiss.
The absence of biotite in rocks of suitable bulk composition suggests temperatures below ca. 400 °C. The Bayındır Nappe was deformed by the syn-metamorphic DA3 event, which is the first deformation event recorded in this tectonic unit. The corresponding SA3 foliation is penetrative and associated with a finegrained, N-trending stretching lineation, LA3 (Figs. 29 and 32). LA3 is expressed by stretched quartz, albite, and chlorite aggregates and aligned tourmaline. In the structurally highest parts of the Bayındır Nappe north of Aydın (see Fig.