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肖板金矿床属受构造控制的中低温岩浆热液矿床，矿化类型为构造蚀变岩型。金多呈独立金矿物形式出现，少许呈分散状；金矿物以自然金为主，平均成色９３０，有少量银金矿和碲金矿。金矿物以包体金、裂隙金、连生金和粒间金等形式嵌布于黄铁矿、黄铜矿、石英、方铅矿及方解石等主要载金矿物中，且石英、方解石中较金属硫化物中占优势。金矿物形态各异，粒度以中细粒为主。
The Xiaopan gold deposit belongs to the moderate-low-temperature magmatic hydrothermal deposit controlled by tectonics. The mineralization type is tectonic altered rock type. Mostly gold appears in the form of independent gold minerals, with a slight dispersion. The gold minerals are mainly natural gold with an average fineness of 930 and a small amount of silver, gold and tellurium gold. The gold minerals are embedded in the main gold-bearing minerals such as pyrite, chalcopyrite, quartz, galena and calcite in the form of inclusions of gold, fissured gold, grained gold and intergranular gold, etc., and the contents of quartz, calcite Metal sulphides dominate. Different forms of gold minerals, fine-grained-based.