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Horzum kurşun Çinko yatakları Kozan-Feke ilçeleri arasında yer almaktadır. Cevherleşme K-G yönlü yaklaşık 20 km boyunca devam etmektedir. Kurşun çinko cevherleşmesi kristalize kireçtaşları, dolomit ve dolomititik kireçtaşlarından oluşan orta Kambriyen yaşlı Çaltepe formasyonuna ait açık renkli kireçtaşları içinde bulunmakta, cevheleşmenin genel duruşu KD-GB doğrultulu ve GD’ye eğimli olarak gözlenmektedir. Cevherleşme kristalize kireçtaşları, dolomit ve dolomititik kireçtaşlarından oluşan orta Kambriyen yaşlı Çaltepe formasyonuna ait açık renkli kireçtaşları içinde bulunmaktadır. Cevherleşmede birincil sülfürlü mineraller galenit, sfalerit, pirit ve az miktarda kalkopirittir. Oksitlenmiş cevher zonunda ise hidrozinkit, simitsonit, götit, limonit ve az oranda serüzit mineralleri gelişmiştir. Blok model yöntemiyle yapılan hesaplamalarda Horzum Kurşun-Çinko yatağında %5 üzeri tenörde 108000 ton cevher rezervi tespiti edilmiştir.
The chickens of the chickens of the chickens of the chickens of the chickens of the chickens of the chickens. The rotating continues for about 20 km in the direction of K-G. The bullet's zinc curvation is found in the light-colored curvations of the middle Cambrian old Chaltepe formation, consisting of crystallized curvations, dolomite and dolomitic curvations, the general position of curvation is observed in the direction of KD-GB and inclined to GD. The convergence is found in the clear-colored convergences of the middle Cambrian old Chaltepe formation, consisting of crystallized curtains, dolomite and dolomite curtains. The primary sulfuric minerals in coverving are galenite, sfalerite, pirite and a small amount of calcopyrite. In the oxidated cabbage zone, hydrozinkite, simitsonite, cabbage, lemonite and a small amount of serozyte minerals have developed. In the calculations made by the block model method, more than 5 percent of the Horzum Bulşun-Zinko bed has been found in the tenor of 108,000 tons of cider reserve.
Horzum lead Zinc deposits are located between Kozan-Feke districts. Mineralization continues for about 20 km in N-S direction. Lead zinc mineralization is within the light colored limestones belonging to middle Cambrian aged Çaltepe formation consisting of crystallized limestones, dolomite and dolomitic limestones, and the general elongation of the mineralization is observed in NE-SW direction and inclination to SE. Mineralization is located within the light colored limestones of the medium Cambrian aged Çaltepe formation consisting of crystallized limestones, dolomite and dolomititic limestones. Primary sulphide minerals in mineralization; galenite, sphalerite, pyrite and few photographs are chalcopyrite. In the oxidized ore zone, hydrozinkite, simitsonite, goethite, limonite and fewer serusite minerals have developed. In the calculations made with the block model method, 108000 tons of reserve was determined in 5% higher grade in Horzum Lead - Zinc bed.
Field : Mühendislik
Journal Type : Ulusal
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