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羊拉铜矿是位于金沙江构造结合带中段,与兰坪陆块东缘维西-绿春晚古生代-中生代火山弧北段(王立全等,1999;李定谋等,2002)交接部位的里农岩体北倾覆端,主要由里农、江边和路农三个矿段组成。羊拉铜矿为区内铜多金属成矿带上典型的后生-叠加作用而形成的斑岩-矽卡岩型铜矿床。羊拉铜矿位于云南省德钦县羊拉乡境内,区内主要出露一套火山-沉积建造。矿区地层由下至上划
The Yangla copper deposit is located in the middle of Jinshajiang structural belt and connected with the Liunong rock at the junction of the Weixi-Lvchun Late Paleozoic-Mesozoic volcanic arc (Wang et al., 1999; Li Dingmou et al., 2002) Body North overturned cover, mainly by the farmers, waterfront and road farmers composed of three mines. The Yangla copper deposit is a porphyry-skarn type copper deposit formed by the typical epigenetic-superimposing action of the copper polymetallic metallogenic belt in the area. Yang pull copper mine is located in Yunnan Province Deqin County sheep Township territory, mainly exposed a volcano - sedimentary construction. Mining strata from bottom to top