The Great Dyke of Zimbabwe intruded into Zimbabwe craton in Late Archean, formed the present structure of five secondary magma chambers located in north and south sectors. Based on the geochemical analysis on the primary ore-bearing beds and sulfide zone and in combination with field geological data, the authors summarized the characteristics and origins of Pt-Pd ore deposit, regarded that the primitive magma of the deposit was derived from the deep mantle, intruded up into the present location in Late Archean, formed the present deposit through crystallization and differentiation.