摘要：扎西康锑多金属矿床位于北喜马拉雅锑金多金属成矿带，是该成矿带上目前发现的唯一的超大型矿床。关于其矿床成因存在诸多争论，有热泉成因（孟祥金等，2008）、地热卤水成因（张建芳等，20101、岩浆热液成因（王艺云等，2012）和海底喷流沉积-改造成因（郑有业等，2012）。
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