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西秦岭造山带的金矿床一般可划分为卡林型与类卡林型(造山型)两类(Mao,2002;陈衍景等,2004;Zhu et al.,2010)。造山型金矿床一般产于西秦岭北成矿亚带的礼-凤古生代盆地中,矿体主要赋存于浅变质的碳酸盐-碎屑岩建造中,并受剪切带、隐爆角砾岩和张性断裂控制。近来,在西秦岭北缘,祁连造山带与秦岭造山带交接的
The gold deposits in the West Qinling orogenic belt can generally be divided into Carlin-type and Carlin-type (orogeny) types (Mao 2002; Chen et al 2004; Zhu et al. 2010). Orogenic gold deposits are generally found in the Li-Feng Paleozoic basin of the North Metallogenic Belt in the West Qinling. The ore body mainly occurs in the construction of super-metamorphic carbonate-clastic rocks and is subjected to shear banding and cryptoexplosive angle Conglomerate and tension fracture control. Recently, in the northern margin of the Western Qinling Mountains, the Qilian orogenic belt and the Qinling orogenic belt handover