烂泥塘铜矿床位于云南省香格里县城,地处印支期义敦-中甸岛弧带南段。区域主要出露有上晚古生代、二叠系、三叠系地层和零星分布的第四系,其中分布最广泛的为三叠系地层。区内具有十分发育的褶皱和断裂,其中控制沉积建造、变质作用、岩浆活动及其有关金属矿产的形成主要是由一系列NNW向紧密线性褶皱和同向断裂组成,容矿构造则是发育的次级断裂和褶皱。该区侵入岩、喷出岩均有出露,它们大部分分布在区域性深大断裂带两侧,其它地区有零星产出,区内中酸性岩分布广, Rotten mud Tongcui deposit is located in Shangri-La County, Yunnan Province, is located in the Indo-South section of Yidun - Zhongdian Island arc. The area is mainly exposed late Paleozoic, Permian, Triassic strata and sporadic Quaternary, of which the most widely distributed Triassic strata. There are well-developed folds and faults in the area, of which sedimentary control, depositional metamorphism, magmatic activity and the formation of the related metallogenic minerals are mainly composed of a series of NNW tight linear folds and syn-faults, while the ore-hosting structures are developed Secondary rupture and folds. The intrusive rocks and the extrusive rocks in this area are all exposed. Most of them are located on both sides of the regional deep fault zone with sporadic output in other areas,