ANTIMONY and mercury deposits are very rich in China. But, most of them are located in the Yangtzeplatform and its neighboring area (Zhang Yuxu et al., 1996). It is usually considered that the Sb, Hgmineralizations have no relations to magmatism. The main genetic types of Sb, Hg deposits are hydrothermal and stratabound-hydrothermal (Liu Lansheng et al., 1996). If the orebodies cut through strata, the deposits are considered hydrothermal; if theorebodies are bedded or lenses paralell to strata, the deposits are considered stratabound-hydrothermal type. Sb often forms independent deposits, such as Xikuangshan deposit, western Hunan. And in a greatnumber of deposits, Sb and other metallic elements were mineralized together, such as Sn-Sb-Pb-Zn-Agin Dachang ore-field, northern Guangxi; W-Sb-Au in Woxi deposit, western Hunan; Sb-Pb-Zn inWuyu, northewestern Guangxi. ANTIMONY and mercury deposits are very rich in China. But, most of them are located in the Yangtzeplatform and its neighboring area (Zhang Yuxu et al., 1996). It is usually considered that the Sb, Hgmineralizations have no relations to magmatism. main genetic types of Sb, Hg deposits are hydrothermal and stratabound-hydrothermal (Liu Lansheng et al., 1996). If the orebodies cut through strata, the deposits are considered hydrothermal; if theorebodies are bedded or lenses paralell to strata, the deposits are Considered stratabound-hydrothermal type. Sb often forms independent deposits, such as Xikuangshan deposit, western Hunan. And in a great number of deposits, Sb and other metallic elements were mineralized together, such as Sn-Sb-Pb-Zn- Agin Dachang ore- field, northern Guangxi; W-Sb-Au in Woxi deposit, western Hunan; Sb-Pb-Zn inWuyu, northewestern Guangxi.