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通过秦岭金矿区域成矿地质条件研究取得的进展 :八卦庙矿区发育有条带状的热水沉积岩 ,金矿床类型属于热水沉积韧性剪切带改造型 ,矿化类型为细脉浸染型 ;马鞍桥金矿的成矿大地构造环境属于华北板块南缘 ,含矿岩系为早古生代的深水斜坡浊积岩相 ,矿区的“浅色岩相”系变质成因 ;煎茶岭金矿属构造蚀变岩型金矿 ,而非超基性岩浆热液型金矿。以上研究为秦岭地区金矿找矿指出了新方向和新类型
According to the research progress of the metallogenic geological conditions in the Qinling gold deposit area, there are strip-shaped hydrothermal sedimentary rocks in the Baguamiao mining area, the gold deposit belongs to the hydrothermal sedimentary ductile shear zone, and the mineralization type is vein disseminated. The metallogenic tectonic environment of the Ma’anshan gold deposit belongs to the southern margin of the North China plate. The ore-bearing rocks are deep-seated turbidite facies of the Early Paleozoic and the “light-colored facies” of the mine area are metamorphic. The Jianchaling gold deposit Variable rock gold, rather than ultrabasic magmatic hydrothermal gold. The above studies have pointed out new directions and new types of gold deposits in the Qinling area