Abstract
It has concluded that the provenance of antimony ore in western Guizhou are as follows together with the previous researches: 1) the mineralization of antimony in western Guizhou is a long, complex process with different sources in various stages. 2) the main sources of antimony may differ in areas. Metallogenic material is provided for the formation of antimony by the “Dachang Layer” and “hydrothermal process”, the area overlapped by both is beneficial for forming antimony with high grade. 3) there may be some other factors providing the metallogenic material or participate in the formation of antimony, such as “oil-gas reservoir”, however, further researches are still needed.
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