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讨论了贵州雷公山地区锑矿的成矿背景、矿床地质特征、成矿机理和成矿规律 ,特别详述了不同级次构造对锑矿带、矿田、矿床、矿体的控制作用。指出在江南造山带古隆起区 ,高密度幔源液体分异的热液活动 ,可能形成石英脉型Sb -Au矿或Sb -多金属矿 ,即与过渡性韧性剪切带有关的蚀变糜棱岩型Au矿或An -多金属矿成矿系列。
The authors discuss the metallogenic background, mineralogical characteristics, metallogenic mechanism and metallogenic regularity of antimony deposits in the area of Leigong Mountain, Guizhou. The controllability of antimony ore belts, ore fields, ore deposits and ore bodies by different levels of structures is especially elaborated. It is pointed out that quartz-vein type Sb-Au ore or Sb-polymetallic ore may be formed in the hydrothermal fluid with high-density mantle source differentiation in the paleo-uplift area of the Jiangnan orogenic belt, ie, the altered temperate zone associated with the transitional ductile shear zone Prismatic Au deposit or An - polymetallic deposit metallogenic series.