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查个勒铜铅锌矿床位于中冈底斯成矿带的中西部,该带东西延伸超过600 km。受印度板块向中国大陆俯冲影响,带内的铅锌矿床多具有东西向成带的特点(张长青,2014)。其中,该带东段发现的一批中大型铜多金属矿床(亚贵拉、洞中松多、洞中拉等)的研究程度相对较高(唐菊兴等,2009;王立强等,2010;费光春等,2010;高顺宝等,2012),而西部的勘查工作刚刚开始,研究程度极低,尤其是对西部矿床的成矿条件、矿床成因还缺乏明确的认识。查个勒是目前在该带中西段发现的唯一确
The Gelehe Cu-Pb-Zn deposit is located in the central-western part of the Middle Gangdese metallogenic belt and extends beyond 600 km. Affected by the subduction of the Indian plate to the mainland China, most of the lead-zinc deposits in the belt have the characteristics of east-west banding (Zhang Changqing, 2014). Among them, a large number of large-scale copper-polymetallic deposits (Yaquila, holes in the cave, holes in the hole, etc.) were found in the eastern part of the belt with relatively high degree of research (Tang Juxing et al., 2009; Wang Liqiang et al., 2010; Fei Guangchun et al , 2010; Gao Shunbao et al., 2012). However, exploration work in the west has just begun and the research level is extremely low. In particular, there is a lack of clear understanding of the metallogenic conditions and genesis of the ore deposits in the western region. Check Le Le is currently found in the band with the only confirmed