Abstract: As a meso-and epi-hydrothermal deposit, the North Zhusilenghaierhan zinc-lead-gold-silver-copper deposit occurred in the Permian granodiorite, granite porphyry and the inner contact zone of surrounding rock. In the course of ore bodies formation, the Permian granodiorite provides the hydrothermal fluid and mineralization substances. The northwest-southeast trending faults offered a channel for granite porphyry intrusion and ore-forming hydrothermal fluid. Nearby ZhusilengHai'erhan,we can still find similar Permian igneous activity and faults. So these areas may exist the similar zinc-lead-gold-silver-copper deposit, and have a good mineralization potentiality.