摘要
The Leipingyan lead-zinc deposit is discovered in the skarn which is formed from the Lower Cambrian Xikou Formation of Triassic calcareous sandstone and quartz diorite. It belongs to the skarn-type mineral deposit in Youxi County, which surface in lead-zinc ores and deep in zinc ore body mainly. The occurrence of orebody and the skarn is close to conformity with irregular, lenticular and veinlike. The lead-zinc ores body with NE rift tectonic and Cu, Pb, Zn, Ag anomalies of soil geochemical have a better telescoping.