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    中亚成矿域斑岩铜(钼)矿带的认识与建立

    Knowledge of porphyry Cu (Mo) ore belts in the Central Asian metallogenic domain and their establishment

    • 摘要: 提要:对中亚成矿域斑岩铜(钼)矿带的认识,起源于哈萨克斯坦滨巴尔喀什—伊犁火山侵入岩带的划分和地球物理场的确认。尤其是对哈萨克斯坦—准噶尔环状磁力异常带的厘定,奠定了中亚成矿域斑岩铜(钼)矿带的地球物理基础和与哈萨克斯坦—准噶尔地块外缘火山-侵入岩带的耦合关系,最终建立起哈—中—蒙中亚成矿域斑岩型铜(钼)矿带的雏型。

       

      Abstract: Abstract:Knowledge of the porphyry Cu (Mo) ore belts in the Central Asian metallogenic domain originates from the division of the peri-Balkhash-Ili volcanic-intrusive belt in Kazakhstan and confirmation by the geophysical field. Through the definition of the Kazakhstan-Junggar ring-shaped magnetic anomaly zone, the authors lay a geophysical foundation of the porphyry Cu (Mo) ore belts of the Central Asian metallogenic domain and recognize their coupling relation to the volcanic-intrusive belts at peripheries of the Kazakhstan-Junggar block. On that basis, an embryo of the porphyry Cu (Mo) ore belts in the Kazakhstan-China-Mongolia Central Asian metallogenic domain is established.

       

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