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矿区位于内蒙~兴安地槽褶皱系北段,岩浆岩发育并多期次侵入活动,断裂构造,火山构造发育,有利于成矿。中生代的构造活动以强烈的断块活动为特征,构造活动也伴随有强烈的燕山期岩浆侵位和火山喷发活动,强烈的燕山期侵入活动也伴随着成矿作用。目前所发现的矿床(点)或矿化活动都与本期的侵入活动有密切联系。在对该区地质、地球物理与地球化学特征综合研究的基础上,利用物化探相关数据,总结该区成矿规律。对矿源和成矿机制进行了探讨,认为与燕山晚期中酸性侵入岩及火山岩有关的火山构造很多,长期的、多期次的北北东向、北东向构造-岩浆活动带有利于含矿源岩的活动,本区应该存在较具规模的热液型或斑岩型Ag、Cu、Pb、Zn、Mo、矿床,具有很好的找矿前景和较大的资源潜力。
The ore area is located in the northern part of the Xing’an diagenetic fold system in the Inner Mongolia area. The magmatic rocks develop and have multiple times of intrusive activity. The fault structure and volcano tectonics are favorable for metallogenesis. The Mesozoic tectonic activities are characterized by strong faulting activities. The tectonic activities are also accompanied by intense Yanshanian magmatic emplacement and volcanic eruptions. Strong Yanshanian intrusions are also accompanied by mineralization. The deposits (spots) or mineralization activities so far discovered are closely related to the current period of intrusion. Based on the comprehensive study of geology, geophysics and geochemistry in the area, the related data of geophysical and geochemical exploration are used to summarize the metallogenic regularity in this area. Based on the exploration of mineral resources and metallogenic mechanism, it is concluded that there are many volcanoes related to the late Yanshanian intermediate-acid intrusive rocks and volcanic rocks. The long-term and multi-phase north-north-east and northeast tectono- magmatic activity belts are favorable to ore-bearing sources Rock activity, there should be more large-scale hydrothermal or porphyry-type Ag, Cu, Pb, Zn and Mo deposits in this area, which has good prospects for prospecting and great resource potential.