黑龙江金厂斑岩型铜金矿床为一特大型铜金矿床,位于黑龙江省东宁县,大地构造位置属兴蒙造山带东段,兴凯地块西南部,位于Ⅲ级构造单元张广才岭-太平岭边缘隆起带中的太平岭隆起与老黑山断陷结合部位。矿区内大面积分布中生代侵入岩,主要为印支期-燕山期中酸性侵入岩,成矿作用与太平洋板块的俯冲作用密切 Located in Dongning County, Heilongjiang Province, the gold plant porphyry copper-gold deposit in Heilongjiang is a large-scale copper-gold deposit located in the eastern part of the Xingmeng orogenic belt and southwest of the Xingkai block. It is located at the level Ⅲ structural unit of Zhangguangcailing-Taiping The Taiping Ridge uplift in the edge of the ridge and the junction of the old Montenegro fault. Mesozoic intrusive rocks are widely distributed in the mining area, mainly during the Indosinian-Yanshanian intermediate-acid intrusive rocks, and the mineralization is closely related to the subduction of the Pacific plate