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世界上大型和超大型内生金矿床与构造关系密切。在92％的矿床上,矿石和金赋存在不同类型的裂隙断裂中;在剩余8％的矿床上,矿石呈浸染状而赋存在爆破角砾岩筒和火山口中以及小侵入岩株中,有时还赋存在含碳页岩和被容矿断裂破坏的某些碳酸盐岩层中。根据构造关系,大型金矿划分为6类:(1)与含矿断裂有关的矿床;(2)与众多延伸稳定的含矿雁行断裂系有关的矿床;(3)延伸稳定且互相靠近的断裂系中的矿床;(4)与相交的含矿裂隙束有关的矿床;(5)与小岩株、脆性岩墙和爆破角砾岩岩体、火山口有空间联系的矿床;(6)与使花岗岩类(花岗片麻岩)岩体构造变形接触带复杂化的含矿裂隙束有关的矿床。
The world’s large and very large endogenous gold deposits are closely related to tectonics. In 92% of the deposits, there are different types of fissures and fractures in ore and gold deposits; in the remaining 8% of the deposits, the ore is disseminated and occurs in blasting breccia pipes and craters and in small intrusive rocks and sometimes It also occurs in carbonaceous shale and some of the carbonate layers damaged by ore-hosting faults. According to the tectonic relationship, the large-scale gold deposits are divided into six categories: (1) deposits related to ore-bearing faults; (2) deposits related to many extended and stable ore-bearing geese; and (3) (4) deposits related to intersected ore-bearing fractures; (5) deposits associated with small rock masses, brittle dikes and explosive breccia rocks and volcano crater; (6) Granite-type (granitic gneiss) rock deformation contact zone complex ore-bearing fractured beam-related deposits.