金矿密集带位于太古宙中朝古陆板块与元古宙蒙古海板块之间的缝合线上，受北西向的富尔河－古洞河岩石圈断裂带控制。金矿床普遍产在上述相邻二板块构造的边缘，与成矿有关的中酸性侵入杂岩体多为深熔花岗岩浆的产物，容矿构造往往为韧性剪切带或脆性构造破碎带内的片理化带。金矿床主要为少硫化物型，次为构造蚀变岩型，该带有优异的成矿条件，是吉林省金矿的主要远景区。 The gold-bearing belt is located on the suture between the Archean Middle Proterozoic Paleo-Proterozoic Mongolia Plate and the Archean, and controlled by the northwesterly Furukawa-Kwu Tung River lithospheric fault zone. The gold deposits are generally produced at the margin of the above two adjacent plate tectonics. Most of the intermediate-acid intrusive complex rocks associated with ore-forming are the products of the deep-melt granite magma. The ore-hosting structures are often in the ductile shear zone or in the brittle structural crust Physical and chemical strip. The gold deposits are mainly of low sulfide type, and the second is tectonic altered rock type. This gold deposit has excellent metallogenic conditions and is the main prospect of gold deposits in Jilin Province.