Özet:

The boxing bed is located in the carcassy hole that has developed over the Senomaniyen old Katrangediya formation, on which the Senoniyen old Birds formation belongs. Diabaz/doleritis, serpanthinitis, radiolaritis, curcumin and square represented and the allocton-located officolithic divisions of the Bozkır unity, which is located in Late Eosen- Early Miyosen, cover this unit with tectonic touch. In this study, which aims to determine the stone type that may be a source of oxides; the analysis results of the samples collected from the oxides and the carbonates, terra-rosas and officyolithic stones that may be a source of them are subject to geochemical and geo-statistic assessment. According to studies conducted in the officolite from potential sources, the high positive relationship between the Al2O3-CaO pair shows that the constant element ratio is different from the boxites, and the deviation from the origin of the regression correctness in the distribution diagrams that these stones cannot lead to the boxites. As the assumption is that the oxides are derived from the curtains, a intermittent product is required to explain the behavior of some elements geochemically. During the process of terra-rosa formation from the cortex, Si and K 77, Zr 60, Ti 50.5, Fe 45.5, Al, Cu, Ga, Nb and Th 37-40, Pb 21, Cr 19.6, Na 14, V 11, Ni 9.3, MG 7.5 and Zn increased 2.5 times and Ca fell 20.1 times. In the process of the transition from Terra-Rose to Boxite; Ca 30.7, Mg26.5, Na 17.9, Si 11, Zn 13.8, Cu 8.7, K 8.6 and P's 7. Despite its decrease 5 times, Al 3.04, Fe 2.14, Ti, Cr and Th increased about 2.5 times, Ga, Nb, Pb and Zr 1.7-2 and V 1.5 times. The high positive, found between Al-Fe and Al-Si in carbonated rockets and terra-roses deriving from them, high negative relationships between Ca-Al, Ca-Si and Ca-Ti elements pairs indicate that Al, Fe, Si, Ti and Ca come from different sources, and coeffective correlation dendograms support the depth. The constant elementaries of carbonate rockets, terra-rows and boxites (Al/Ti, Al/Th, Al/Zr, Ti/Zr, Ti/Ga, Ti/Nb, Ti/Th, Ga/Nb, Ga/Th, Ga/Zr, Nb/Th, Nb/Zr, Th/Zr) are similar to each other, while the offical rockets are different. In the correlation analysis, in which the oxides and potential sources were evaluated together, Al-Fe, Al-Ti, Al-Ga, Al-Nb, Al-Th, Al-Zr, Ti-Ga, Ti-Nb, Ti-Th, Ti-V, Ti-Zr, Ga-Nb, Ga-Th, GaZr, Nb-Th, Nb-Zr and Th-Zr elements pair were determined to have a very high positive relationship (>0.95). In the distribution diagrams of these elements, regression also passes directly from the center or very close to the center, terra-rosas offer a distribution between boxites and carbonate stones and officyolites. According to these data, it can be said that the separation product, which is necessary for the formation of boxite from the coatings, is widely observed on the carbonate rocks of all the Toros generations and is the terra-roses that continue to form even today.

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