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矿床位于额尔古纳地块与松嫩地块陆陆碰撞带塔源—兴隆早加里东造山带北东端,处在古生代隆起与中生代火山盆地交接带附近的瓦拉里—北西里铁、金成矿亚带,具有晚印支期和晚燕山期二期成矿特点,以晚印支期变质热液成矿为主。
The ore deposit is located between the Argonaut block and the Songnen-Nenneh continent, the source of the Ta-source-Xinglong Long-Caledonian orogenic belt at the north-eastern end. It is located between the Paleozoic uplift and the Walari-North Xili iron near the transition zone of the Mesozoic volcanic basin, Gold mineralization belt, with late Indosinian and late Yanshan Stage II metallogenic characteristics, mainly to late Indosinian metamorphic hydrothermal mineralization.