CRUSTAL PROCESS IMPLICATIONS FOR A TECTONO-MAGMATIC EVOLUTION OF LATE CENOZOIC EGRIGOZ PLUTON IN WESTERN ANATOLIA (TURKEY)
The Late Cenozoic igneous province in western Anatolia is one of best examples of magmatism within continental crust that has been thickened and then thinned by orogenic processes. The Egrigöz pluton is the one of the largest and least-understood pluton. It emplaced at high crustal levels (Ozgenc and Ilbeyli 2008). The rocks have a compositional range from granodiorite to granite. They are high-K calc-alkaline and having I-type characteristics. They show linear and continuous trends in Harker diagrams (Ozgenc and Ilbeyli 2008). Linear trends can be caused by numerous petrogenetic processes, such as crustal contamination, mixing, crystal fractionation and partial melting (Cox et al. 1987; Wilson 1991). Field and geochemical characteristics of the pluton indicate an origin through partial melting of mafic lower crustal source rocks. In western Anatolia, the melt generation mechanism for the intrusive rocks could be crustal extension and uplift following collision.
References
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