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五道岭钼矿床赋存于晚印支期白岗质花岗岩与上二叠统五道岭组上段中部凝灰质砂岩及流纹质凝灰岩接触挤压带的矽卡岩中。矿体的形态、规模、产状严格受矽卡岩带控制,钼矿体的形成与侵入接触挤压带的矽卡岩密切相关。具有典型的矽卡岩型矿床特征。
The Wudaoling molybdenum deposit occurs in the skarn in contact with the crustal tuff and rhyolitic tuff in the Late Indosinian Baigang granite and the Upper Permian Wudaoling Formation. The morphology, scale and occurrence of the ore body are strictly controlled by skarn zones. The formation of molybdenum ore bodies is closely related to the skarn intruding into the extrusion belt. With a typical skarn-type deposit characteristics.