塔拉特铅锌矿床是产于新疆南阿尔泰晚古生代克兰火山沉积盆地众多矿床中的一个,目前已达中型规模。对该矿的成因认识仍存在争议,有强调火山沉积特征的火山喷流沉积型(康吉昌等,2009;袁建江等,2011)和注重岩浆热液蚀变特征的矽卡岩型(李登峰等,2013)等不同观点。本文综合研究矿床地质特征并结合同位素特征研究探讨了该矿床的成因机制。 Talat lead-zinc deposits are produced in the late Paleozoic Kelan volcanic sedimentary basin in southern Altay, Xinjiang, and have reached a medium scale. The origin of the mine is still controversial. There are volcanic jet depositional types (Kang Jichang et al., 2009; Yuan Jianjiang et al., 2011) that emphasize volcanic sedimentary features and skarn-type that focuses on magmatic hydrothermal alteration (Li et al. 2013) and other different points of view. This paper comprehensively studies the geological characteristics of the deposit and studies the genesis mechanism of the deposit in combination with isotopic characteristics.