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马头滩金矿床赋存于晚古生代中酸性火山岩中，受脆韧性剪切带控制，成矿年龄与控矿的糜棱岩带的形成时代相近，成矿物质主要来自围岩火山岩，成矿流体由变质水和大气降水溶液组成。这些特征说明该矿床与剪切带之间存在时－空和成因联系，是一个典型的韧性剪切带型金矿床。
Ma Toutan gold deposit occurs in the Late Paleozoic intermediate-acidic volcanic rocks and is controlled by brittle-ductile shear zones. The metallogenic ages are similar to those of the mylonitized ore belts. The metallogenic materials mainly come from the surrounding volcanic rocks, mineralization Fluid consists of metamorphic water and atmospheric precipitation solution. These characteristics indicate that there is a time-space-genesis relationship between the deposit and the shear zone and is a typical ductile shear zone type gold deposit.