S. KADİR Et Al. , "The occuurence of the hydrothermal Karaçayır kaolinite deposit within Neogene volcanites and Paleozoic schists, Uşak (Western Anatolia), Turkey," International Conference Clays, Clay Minerals and Layered Materials-CMLM2009 , Zvenigorod, pp.251, 2009
KADİR, S. Et Al. 2009. The occuurence of the hydrothermal Karaçayır kaolinite deposit within Neogene volcanites and Paleozoic schists, Uşak (Western Anatolia), Turkey. International Conference Clays, Clay Minerals and Layered Materials-CMLM2009 , (Zvenigorod) , 251.
KADİR, S., ERKOYUN, H., & ERMAN, H., (2009). The occuurence of the hydrothermal Karaçayır kaolinite deposit within Neogene volcanites and Paleozoic schists, Uşak (Western Anatolia), Turkey . International Conference Clays, Clay Minerals and Layered Materials-CMLM2009 (pp.251). Zvenigorod
KADİR, SELAHATTİN, HÜLYA ERKOYUN, And HANDE ERMAN. "The occuurence of the hydrothermal Karaçayır kaolinite deposit within Neogene volcanites and Paleozoic schists, Uşak (Western Anatolia), Turkey," International Conference Clays, Clay Minerals and Layered Materials-CMLM2009, Zvenigorod, 2009
KADİR, SELAHATTİN Et Al. "The occuurence of the hydrothermal Karaçayır kaolinite deposit within Neogene volcanites and Paleozoic schists, Uşak (Western Anatolia), Turkey." International Conference Clays, Clay Minerals and Layered Materials-CMLM2009 , Zvenigorod, pp.251, 2009
KADİR, S. ERKOYUN, H. And ERMAN, H. (2009) . "The occuurence of the hydrothermal Karaçayır kaolinite deposit within Neogene volcanites and Paleozoic schists, Uşak (Western Anatolia), Turkey." International Conference Clays, Clay Minerals and Layered Materials-CMLM2009 , Zvenigorod, p.251.
@conferencepaper{conferencepaper, author={SELAHATTİN KADİR Et Al. }, title={The occuurence of the hydrothermal Karaçayır kaolinite deposit within Neogene volcanites and Paleozoic schists, Uşak (Western Anatolia), Turkey}, congress name={International Conference Clays, Clay Minerals and Layered Materials-CMLM2009}, city={Zvenigorod}, country={}, year={2009}, pages={251} }