斑岩铜矿资源在我国占重要地位,并有广泛分布。斑岩铜矿矿化经常是以地槽区造山晚期和构造稳定断块中火山盆地边缘为特征,矿化岩体受背斜轴和构造鼻或两组断裂控制。这些岩体是属具斑状结构浅成岩体,或似斑状结构中浅成岩体。矿化集中于侵入体流动前缘及其两侧陡变缓部位,或发生在岩株、岩 Porphyry copper resources occupy an important position in our country, and are widely distributed. The porphyry copper mineralization is often characterized by late volcanic orogeny and tectonically-stable volcanic basins in the terrane area, where the mineralized rock bodies are controlled by the anticline and structural nose or two sets of faults. These rocks are porphyritic epithermal bodies, or porphyritic structures of epithermal bodies. Mineralization is concentrated in the front of the invade and on both sides of the steep gentle transitional site, or in the rock, rock