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Thermal Structure of Continental Crust in Central Anatolia
Central Anatolia Region located in Alp-Himalaya orogenic belt, consist of continental blocks which have a history of different metamorphism and deformation. These blocks are seperated by ophiolitic suture belts represented old oceanic crust and mantle.
These complex evoluation of the region are reflected to its thermal properties, high and low heat flow regions are located side by side. From these point of view, the region between Kırşehir and Nevşehir provinces indicate interesting thermal structure for the purposes of mesured heat flow values.
In this study, two dimentional heat flow modelling has been calculated along a line of which is about 140 km located in between Nevşehir and Kırşehir provinces. The depth of the model is 35 km and this value is same with Moho discontinuaty. Temparature depending on the surface heat flow value, in the 35 km crustal mantle is higher as 12500C and in the south part of the model, is lower as 4000C.
SAĞCI Nurcan
Danışman :Yrd. Doç. Dr. Hüseyin TUR
Anabilim Dalı :Jeofizik Mühendisliği
Mezuniyet Yılı :2009
Tez Savunma Jürisi : Yrd. Doç. Dr. Hüseyin TUR
Prof. Dr. İbrahim KARA
Prof. Dr. Ali PINAR
Prof. Dr. Hayrettin KORAL
Yrd. Doç. Dr. Ali İsmet KANLI
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