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闹牛山—巨里河区带位于内蒙东部铜多金属成矿带上。大地构造处于大兴安岭—燕山火山活动带,布特哈旗—多伦火山活动亚带(中亚带)的中部,是一个迭加于晚古生代褶皱基底之上的构造单元(图1)。图1 区带大地构造略图1—Ⅰ级构造单元界线;2—Ⅱ级构造单元界线;3—中新生代陆相盆地
The trouble Niu Shan - Ju Lihe zone is located in eastern Inner Mongolia copper polymetallic metallogenic belt. The tectonic setting is located in the middle part of the Daxinganling-Yanshan volcanic activity belt and the Buteha-Duolun volcanic activity sub-belt (Central Asia Belt), which is a tectonic unit superimposed on the Late Paleozoic fold basement (Figure 1). Fig.1 Schematic diagram of regional geotectonic belt Line 1-Ⅰ tectonic unit boundaries; boundary line 2-Ⅱ tectonic units; 3-Mesozoic-Cenozoic continental basin