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邓格在高硫石英脉型金矿床产于胶东东部牟平—乳山金成矿区中部北北东向金牛山断裂的次一级平行断裂中，由四条黄铁矿—石英脉组成。笔者对该矿床金矿物的特征、金的赋存状态和富集规律、及主要载金矿物—黄铁矿、黄铜矿、方铅矿、毒砂、石英等的产出特征、物理性质、化学成分及其它特征进行了叙述。金主要呈金—银固溶体系列的独立矿物产出，包括银金矿、自然金和金银矿。黄铁矿为矿石中主要金属矿物，与金关系非常密切，是主要的载金矿物，８０％以上的金分配在黄铁矿中。含金石英脉与不含金石英脉中黄铁矿的微量元素含量有明显差别，以此可以区分二者。金与砷（毒砂）有明显的正相关性，在含有毒砂的矿石中几乎都能发现银金矿，所以毒砂可作为寻找此类金矿床的矿物学标志。载金脉石英为灰色透明，ＳｉＯ＿２含量较低，杂质含量较高，黄铁矿具有碎裂结构，热电系数为正值（Ｐ型），黄铜矿热电系数为高负值，它们为载金矿物的标型。
DENG Ge is composed of four pyrite-quartz veins in the sub-first parallel fracture of the North-East-East Jinlian Mountain fault in the Muping-Rushan gold metallogenic area in the eastern part of the Jiaodong high-quartz quartz vein type gold deposit. The author of the deposit characteristics of gold minerals, gold occurrences and enrichment laws, and the main gold-bearing minerals - pyrite, chalcopyrite, galena, arsenopyrite, quartz and other output characteristics, physical properties, Chemical composition and other characteristics are described. Gold is primarily a standalone mineral output of gold-silver solid solution series, including silver and gold, natural gold and gold and silver. Pyrite is the main mineral in the ore, which is closely related to gold and is the main gold-bearing mineral. More than 80% of the gold is distributed in the pyrite. There is a significant difference in the trace element contents of pyrites between the auriferous quartz veins and the non-auriferous quartz veins, so that the two can be distinguished. There is a clear positive correlation between gold and arsenic (arsenopyrite). Almost all silver and gold deposits can be found in arsenopyrite-bearing ores, so arsenopyrite can be used as a mineralogical indicator for finding such gold deposits. Containing gold vein quartz gray transparent, low SiO 2 content, higher impurity content, pyrite has a fragmented structure, the thermoelectric coefficient is positive (P type), chalcopyrite thermoelectric coefficient is a negative value, they are gold Minerals standard.