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本文所研究的矿区分布在昂农-图林带中。该带位于阿金斯克地块西部的蒙古-鄂霍次克构造带的南亚带。该区有元古代、古生代和中生代的沉积岩,侵入岩和喷出岩的出露范围很广。
The mining area studied in this paper is located in the Aung Nong-Tulin Belt. This belt is located in the southern Asian belt of the Mongolian-Okhotsk tectonic belt to the west of the Aguinsk massif. The area has metamorphic, Paleozoic and Mesozoic sedimentary rocks, intrusive rocks and extrusive rock exposed a wide range.