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I.

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8th International Scientific Conference - SGEM2008
Publication

GEOLOGICAL INVESTIGATION OF THE CARIKSARAYLAR - KOZLUCAY AREA (ISPARTA-TURKIYE)

(SGEM Scientific GeoConference, 2008, Y. Bozkir, A. Ayhan, F. Arik)

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The study area is located in southeastern part of Sultandaglari, 50 km to the northeast of Isparta. The geological units exposed in the area are: The Lower-Middle Cambrian Caltepe Formation, which comprises grey and pink coloured recrystallized limestone, nodular limestone, dolomitic limestone and dolomite, is the oldest unit. The Upper Cambrian - Lower Ordovician Seydisehir Formation conformably overlies the Caltepe formation and comprises green to brown coloured metasandstone, quartzite, phyllite, calcshists, sc...

Geology2008
8th International Scientific Conference - SGEM2008
Publication

GEOLOGICAL SETTING AND PETROGRAPHICAL CHARACTERISTICS OF THE BOZKIR OPHIOLITIC MELANGE, BOZKIR (KONYA- TURKEY)

(SGEM Scientific GeoConference, 2008, A. Ozturk, M. M. Karadag, A. Ayhan, F. Arik)

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In the study area the lowermost unit is the autochthonous GeyikdagД± unit (Upper Cambrian-Lower Ordovician Seydisehir Formation, Upper Jurassic Hacialabaz formation, Upper Cretaceous Cokelen diabase and Upper Cretaceous Saytepe formation). The BolkardagД± unit (Devonian-Lower-Middle Carboniferous Hocalar formation, Upper Permian, Taskent formation and Jurassic-Upper Cretaceous SinatdagД± formation) rests allochthonously on the GeyikdagД± Unit. The Bozkir unit (Bozkir melange with ophiolite and (Mahmuttepe limeston...

Geology2008
8th International Scientific Conference - SGEM2008
Publication

GEOLOGY, MINERALOGY AND GEOCHEMICAL CHARACTERISTICS OF THE GOZECUKURU (KUTAHYA) As-Sb DEPOSITS, NW TURKEY

(SGEM Scientific GeoConference, 2008, F. Arik)

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The Goze\ccukuru As-Sb mineralization was occured in an area of 2,1 km2, which is located near the small town of Sahin Village, 22 km west of Kutahya. Low-grade metamorphic rocks (metasandstones, metaconglomerate, chalcshist, graphitic mikaschists, and micaschist and quartz schist) of Upper Paleozoic (Carboniferous- Permian) aged Sahin Formation form the basement. The rhyolitic and rhyodacitic tuffs of Middle-Upper Miocene aged TavsanlД± volcanites uncomformably covers to the Sahin Formation. The Upper Pliocene ag...

Geology2008
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