摘要
The Weibao mining area, located at the Qimantage Paleozoic Era compound trench-arc belt in the Qaidam micro tectonic plate of Tarimu-North China tectonic plate, belongs to the east Kunlun Mountains Fe-Pb-Zn-Cu-Co-Au-W-Sn-asbestos-salts mineralization belt-Qimantage W-Sn-Pb-Zn-Fe-Cu multi-metalliferous ore belt, the Qin-Qi-Kun mountains mineralization territory-Kunlun mountains mineralization province. The ore is mainly with half idiomorphic-xenomorphic-granular metacryst texture and contaminated structure, partially with block structure. Genetic type of the ore deposit is classified into the deposition-magmatic gas fluid superimposition and stratabouned.