摘要
On the view of the alteration mineral assemblage, alteration types and spatial distribution, the ore was a skarn-type ore. The set of alteration is not only directly controlled by the altered rock epiphysis, but also by the eastwest, northwest striking preore faults and lithologic characters. Formed a set of strips away from the contact zone of the skarn, in particular the epidote actinolite skarn is developed much well. The mine mineralization is closely related to the skarns and the generation of ore body is later than the skarn, not only skarn- and ore-body shape can be coincided, but skarn ore body or vein also formed independently.