霍洛台Ⅰ区南铜钼矿床位于大兴安岭中北段的铁、铜、金、钼、钨成矿区（带）上，其成矿阶段由早至晚分为4个阶段：磁铁矿-石英-钾长石阶段（Ⅰ）、石英-辉钼矿阶段（Ⅱ）、石英-多金属硫化物阶段（Ⅲ）、石英-萤石-方解石阶段（Ⅳ）。石英-辉钼矿阶段与石英-多金属硫化物阶段为主要成矿阶段。流体包裹体类型有含CO₂三相包裹体（C型）、含子矿物包裹体（S型）、富气相包裹体（V型）、富液相包裹体（L型）。成矿流体总体属于高盐度的H₂O-NaCl-CO₂体系。该矿床中的辉钼矿主要发育在钾硅化带中，形成于早阶段高温、高盐度流体环境；黄铜矿等金属硫化物主要发育于绢英岩化带中，形成于中温富液相流体环境。辉钼矿的沉淀主要与沸腾作用和温度降低有关，黄铜矿等金属硫化物的沉淀主要由温度降低和大?旌纤隆Ｗ酆戏治鋈衔袈逄Ⅰ区南铜钼矿床为典型的斑岩型矿床。

Copper-molybdenum deposit in the southern Huoluotai AreaⅠare located on the iron,copper,gold,molybdenum and tungsten metallogenic zone(belt) sitting in the central north section of Greater Khingan Mountains.The metallogenic stages are pided into 4 phases in time:stageⅠis magnetite-quartz-potassium feldspar stage,stage Ⅱ is quartz-molybdenite,stageⅢis quartz-polymetallic sulfide,and stage Ⅳ is quartz-fluorite-calcite.Quartz-molybdenite stage and quartz-polymetallic sulfide stage are the main metallogenic stages.The fluid inclusions are mainly composed of CO₂bearing 3phase inclusion(C type),submineralbearing inclusion（S type），gas-rich inclusion（V type），and liquidrich inclusions（L type）.Oreforming fluids generally belong to high salinity H₂O-NaCl-CO₂ system.The molybdenite in the deposit mainly develops in the potassium silicification zone,and was formed in the early stage of high temperature and high salinity fluid environment; polymetallic sulfide like chalcopyrite mainly develops in the sericitization zone,and was formed in the medium temperature liquidrich fluid environment.Molybdenite precipitation is mainly related to boiling and temperature reduction,polymetallic sulfide precipitation like chalcopyrite is mainly caused by temperature reduction and atmospheric water mixing.Comprehensive analysis thinks the copper-molybdenum deposit in the southern Huoluotai AreaⅠis a typical porphyry deposit.