绝大多数金属矿床,地质构造复杂,其勘探深度不断增加,是北方塔吉克斯坦地区采矿工业矿物原料基地今后发展的基本趋向之一。目前正勘探两种类型的矿床:矽卡岩多金属矿床(阿尔金塔布干斯克等矿区)和热液矿床(以卡里曼苏尔为代表的许多矿区)。变质作用、多期硅化和复杂的地质构造,是造成岩石成分驳杂,形成裂隙和断裂交 The vast majority of metal deposits have complicated geological structures and their exploration depth is continuously increasing, which is one of the basic trends for the future development of mineral raw materials bases in northern Tajikistan. Two types of deposits are currently being explored: skarn polymetallic deposits (Archetabu-Bakhstan and other mines) and hydrothermal deposits (many mines represented by Kalimantur). Metamorphism, multi-stage silicification and complex geological structure, is caused by miscellaneous rock composition, the formation of cracks and fracture intersection