地层、侵入岩、断裂构造是工作区内钨矿的三个基本的成矿地质条件。
The stratum, intrusive rock, and faulted structure are three basic ore-forming geology factors of tungsten ore in the work area.
岩浆岩的侵入明显受断裂构造控制。
Magmatic intrusion obviously is controlled by faulted structure.
明确提出了侵入接触带构造控矿的观点，从而为进一步研究其成矿及控矿作用提供必要的理论依据。
The idea that the intrusive contact structure controls the-body will provide theoretical evidence for the further research of mineralization and ore control.
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