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浙、赣、皖相邻地区金属矿产分布呈现南钢金北钨锡的特点。十六条主要线性断 裂带和九岭、怀玉地体的拼接带叠复构成区域一级控矿断裂网络，同期不同类型金属矿化围绕 网络结点处的岩体分布组成矿田尺度斑岩成矿体系，两者分别决定和控制了区域范围和矿田范 围金属矿床包括铜、金矿床的空间就位。燕山期强烈的构造岩浆活动伴随有爆发式的金属成矿 作用，铜、金矿化主要与燕山早期Ｉ型中酸性花岗岩类有关。成矿元素部分来自浅部不同地层， 特别是中元古和中一晚元古界含矿岩石建造，也有来自下地壳以至地幔。德兴铜金矿集区的成 矿地质条件和找矿标志组合在区内独一无二，但其周边地区仍然存在中、大型铜、金矿床的找矿 潜力，四个优选的普查靶区有望发展成铜、金勘查基地。利用成矿的断裂网络层次定位思路和 矿田级富铜、金斑岩体系找矿模型在该区进行铜、金预测一普查、有可能收到事半功倍的效果。
The distribution of metal minerals in the adjacent areas of Zhejiang, Jiangxi and Anhui shows the characteristics of Jindong Jindong tungsten and tin. Sixteen major linear fault zones and JiuLing and Huaiyu terranes are overlapped to form a first-level ore-control fracture network in the region. In the same period, the distribution of rock mass around the network nodes of different types of metal mineralization constitutes ore-scale porphyry The ore system, both of which determine and control the spatial distribution of metal deposits including copper and gold deposits in the regional scope and orefield area, respectively. The strong tectonomagmatic activity of Yanshanian period accompanied by the explosive metallogenic process. Copper and gold mineralization are mainly related to the type I intermediate acidic granitoids in the early Yanshanian. The ore-forming elements are partly derived from different strata in the shallow part, especially the Middle Proterozoic and Middle Proterozoic ore-bearing rocks, and from the lower crust to the mantle. The combination of ore-forming geological conditions and prospecting signs in the Dexing copper-gold area is unique in the area, but there are still potential for prospecting for medium- and large-sized copper and gold deposits in the surrounding areas. The four preferred general survey areas are expected to develop into Copper, gold exploration base. It is possible to get a multiplier effect by using the stratigraphic positioning of the metallogenic fault network and ore prospecting models of copper-rich and gold-porphyry ore-bearing systems in the area for copper and gold prediction.