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1概况本成矿带主要指介于雅鲁藏布江缝合带(IYS)与藏南拆离系主拆离面(STDS)之间的特提斯喜马拉雅的部分,西起噶尔经定日东至隆子,总体呈EW向展布,长约2000km,东宽西窄,北邻冈底斯岩浆成矿带,南为高喜马拉雅地体,隶属于特提斯成矿域—喜马拉雅成矿省—喜马拉雅AuSbFe白云母成矿带—北喜马拉雅(大陆边缘)AuSb白云母成矿亚带,为青藏高原最具特色和最重要的锑-金成矿区带。该矿带已发现锑
1 General The metallogenic belt mainly refers to the part of the Tethys Himalayas between the Yarlung Zangbo suture (IYS) and the main detachment (STDS) of the South Tibet Detachment System. From west to east, It is generally EW-trending with a length of about 2000km and a narrow east-west width and north-west Gangdise magmatic mineralization belt. The south is a high Himalayan terrane and belongs to the Tethys metallogenic domain - the Himalaya metallogenic province - the Himalayan AuSbFe The parent metallogenic belt - AuSb muscovite subband in the northern Himalaya (continental margin) is the most distinctive and important antimony-gold mineralization zone of the Tibetan Plateau. The mine has discovered antimony