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Karahidir-Bozada Tepe Fluorit sahasi hakkinda rapor
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Kaman Bayindir k 6 yU Muazzez Akdeniz fluorit sahasi hakkinda 6 n rapor ( Preliminary report on Muazzez Akdeniz fluorite field in Kaman Bayindir region )
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Determination of fluid inclusion and rare earth element (REE) geochemistry of Bayindir. tsahocali, Yeniyapan and Aligar (Kaman-Kirgehir) fluorites. Third International Turkish Geology Sym
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Cankiri-Corum havzasinin jeolojisi ve petrol kaynaklari (Geology of Cankiri-Corum basin and petroleum possibilities)
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Bayindir fluorit filonlarinin nadir toprak efementleri jeokimyasi (Geochemistry of rare earth elements of Bayindir fluorite veins)
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Determination of fluid inclusion and rare earth element ( REE ) geochemistry of Bayindir . tsahocali , Yeniyapan and Aligar ( Kaman - Kirgehir ) fluorites
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Aligar (Kaman-Kirgehir) fluoritlerinin nadir toprak elementi jeokimyasi (Geochemistry of earth elements of Aligar (Kaman-Kirgehir) fluorites)
Koç Koç, Özmen Özmen (2000)
Bayindir, Isahocali, Yeniyapan and Alişar (Kaman‐Kirşehir) fluoritlerinin sivi kapanim incelemeleri (Fluid inclusion studies of fluorites from Bayindir, Isahocali, Yeniyapan and Alişar (Kaman‐Kirşehir) regions)Journal of the Institute of Science and Technology, Gazi Uni., 13
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Tin silicate-borate-oxide equilibria in skarns and greisens; the system CaO-SnO<2) -SiO<2) -H<2) O-B<2) O<3) -CO<2) -F<2) O<-1)Economic Geology, 73
Kadioǧlu Kadioǧlu, Ve Güleç Ve Güleç (1996)
Agaçören granitoidinde yer alan gabro kütlelerinin yapisal konumu: Jeolojik ve jeofizik (özdirenç) verilerinin yorumu (Structural characteristics of gabbro massive in Aǧaçören granodiorites: Interpretation of geological and geophysical data)Tr. J. Earth Sciences, 5
(1987)
Cefalikdag ve Baranadag pliltonlarinin (Kaman) petrografik ve kimyasal-mineralojik 6zellikleri (Petrographic, chemical and mineralogical characteristics of Cefalikdag and Baranadag plutons
Fluorite mineralization occurs along fractures and cracks of Middle Eocene and Pliocene limestones and marls in the north and northeast of the Pöhrenk region (Çiçekdagi, Kirsehir). Tb/Ca – Tb/La and Y/Ho ratios were obtained from REE contents of fluorites which have revealed that mineralization is of hydrothermal type. Negative Ce anomalies and positive Eu anomalies reflect that hydrothermal solutions once had high oxygen fugacity. Fluid inclusion studies indicate that homogenization temperatures of mineralization varied between 90°C and 200°C, and hydrothermal solutions are composed of NaCl + KCl + MgCl2 + H2O. In addition, salinity measurements show that hydrothermal solutions were mixed with meteoric or rock formation water. Geologic setting, REE geochemistry and fluid inclusion studies suggest that mineralization was deposited from a solution generated by mixing of magmatic and meteoric water under epithermal conditions.
Acta Geologica Sinica (English Edition) – Wiley
Published: Mar 1, 2001
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