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Geology and geochemical properties of Southern Dağardi (Kütahya) Ophiolite

The study area that is Dagardi Region and its southern side is located in Izmir-Ankara Sture Zone in Northwest Anatolia. In basement of the study area, Egrigoz Metamorphic rocks, affected of low degree green schist metamorphism, are found. Ophiolitic melange tectonically overlies Egrigoz Metamorpics. In the region the emplacement age of the ophiolitic rocks are considered from Senomaniyen to Maastrichtian. Egrigoz Granite formed and intruded, associated with the N-S directioned tensional regime in the region of Aegan probably between Oligosen and Miocene. It cut Egrigoz Metamorphics and outhocton limestones, emplaced as a batolite. Neogen aged volcano-sedimentary rocks directly overlie the ultrabasic unit, ophiolitic melange and partially limestones as an angular unconformity. Basic lavas, spilitic diabases and metadiabases indicate the middle ocean ridge region properties with respect to their petrographical, geochemical and field data. Glaucophane and lawsonite existence within the metadiabases, show us, that rocks had been undergone HP/LT metamorphism during the subduction process and necessary about the pressure of 6±2 kb., the temperature of 200-250 o C and nearly at depths of 15-20 km. in conditions. From the results of the chemical analyses of ultrabasic rock, basic lava, diabase rock patterns, all these rocks had been formed from the 5-15 % percentage of mante depletion, low degree of melting and show quartz