Luziyuan Pb-Zn-Fe deposit in Zhenkang of Yunnan is a supersized polymetallic deposit that is discovered in recent years. The ore bodies occur in strata of Shahechang formation of Upper Cambrian system. The occurrence, mineralization and alteration and occurrence environment of ore bodies are obviously controlled by structure of the mining area: the plane distribution of the orebodies is mainly controlled by NE strike brittle fracture structural system, and the shape and distribution of ore bodies are controlled by various sequential structural systems inside the producing formation. Polar stereographic projection method is used in this paper to allocate ore-bearing joints by stages.
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