内蒙古东部陶廷达坂—团结地区内生矿产成矿潜力分析

Analysis of endogenetic mineral resources potential of Taotingdaban-Tuanjie Region,east Inner Mongolia

内蒙古陶廷达坂—团结地区在中生代盆岭构造体系发育、演化过程中,形成了不同类型的构造-岩浆成矿系统,主要有构造-岩浆穹窿型和火山机构型两类;区内的内生矿产是中生代构造-岩浆成矿系统长期活动的产物;内生矿产以矿化集中区形式产出,从成矿规律、控矿因素等方面分析认为区内的内生矿产具有较大成矿潜力。

The Taotingdaban-Tuanjie region has a complex tectonic setting. In the Mesozoic the Basin- Range tectonic system is developed with different tectonic-magmatic ore-forming systems. Structural-magmatic dome and volcanic edifice are the two main systems. Endogenetic mineral resources in this region are the products of the long-term tectonic, magmatic and metallogenic evolution during Mesozoic Era occurring as clustered mineralization areas. Analysis of metallogeny, ore-control factors show that Taotingdaban-Tuanjie region is still potential for further endogenetic mineral resources prospecting.