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西藏曲水县南木乡达布村一带显角囊地区的斑岩型铜钼矿床位于冈底斯岩浆岩带中段的南部,南距雅鲁藏布江结合带约30 km。大地构造位于冈底斯大陆北缘前陆的一部分,即冈底斯-念青唐古拉板片中段南部边缘的冈底斯陆缘火山—岩浆弧的东段,南邻雅鲁藏布江结合带,矿区所处的构造单元位于晚白垩世—中新世结蒲林—夏拉火山岩浆弧中。研究表明,大多数斑岩型铜
The porphyry copper-molybdenum deposit in the Dabu Village, Nan Mu, Tibet, Qushui County, Tibet, is located in the southern part of the middle Gangdise magmatic belt and is about 30 km south of the Yarlung Zangbo River junction belt. The tectonic structure is located in the front part of the northern margin of the Gangdise continent, the eastern part of the margin of the Gangdese Peridoterozoic-Magmatic Arc on the southern margin of the middle section of the Gangdese-Nyainqentanglha plate, and the southern Brahmaputra junction, The tectonic units are located in Late Cretaceous-Miocene knot-Pula-Shala volcanic arc. Research shows that most porphyry type copper