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索尔库都克矿床是近年来新疆境内探明的中型铜(钼)矿床。对其成矿地质环境、矿床地质特征、夕卡岩及其分带的研究表明。该矿床之夕卡岩与Д.С.柯尔仁斯基(1955)所划分的类夕卡岩相类似。该夕卡岩是由凝灰砂岩、安山玢岩等变质形成的。流体包裹体和稳定同位素的研究表明,该矿床是我国特殊的层状夕卡岩矿床,与接触交代夕卡岩矿床明显不同。
The Sorkukduk deposit is a proven medium-sized copper (molybdenum) deposit in Xinjiang in recent years. Studies on its geological environment of mineralization, geological characteristics of deposit, skarn and its zonation show. The skarns of the deposit are similar to the skarn analogues classified by Д.С. Kerrinskiy (1955). The skarn is formed by tuffaceous sandstone, andesite and other metamorphic rocks. Fluid inclusions and stable isotopes indicate that the deposit is a special stratified skarn deposit in China, which is obviously different from the contact skarn deposit.