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彝良县发达铅锌矿地质特征及成因分析

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彝良县发达铅锌矿位于滇、川、黔铅锌(银)成矿带,矿区内发现铅锌矿体5条,矿体主要赋存于NW向、NE向断裂,含矿地层为奥陶系中统大箐组厚层-块状白云岩,矿区控矿因素为"构造+岩性"的构造控矿型式.通过矿石矿物组合关系,判断该铅锌矿成矿过程分为3个阶段.LA-ICP-MS原位微区微量元素含量表明,矿床的成因与岩浆或火山活动有关,而Cd、Tl元素的相对富集,表明该铅锌矿形成的Ⅲ阶段可能是发达铅锌矿的主成矿期.矿床成因属构造+岩性控制的中低温热液交代型铅锌矿床.
Geological Characteristics And Genetic Analysis of Developed Lead-zinc Deposits in Yiliang County
Yiliang County developed lead-zinc ore is located in the Yunnan,Sichuan and Qian lead-zinc(silver)me-tallogenic belt.Five lead-zinc ore bodies are found in the mine.The ore bodies mainly occur in NW and NE trending faults.The ore-bearing strata are thick layer-massive dolomite of Middle Ordovician Daqing Formation.According to the ore-mineral association relationship,the metallogenic process of the lead-zinc deposit can be divided into three stages.The contents of trace elements in LA-ICP-MS in situ indicate that the genesis of the deposit is related to mag-matic or volcanic activities,while the relative enrichment of Cd and Tl elements indicates that the Ⅲ stage of the for-mation of the lead-zinc deposit may be the main metallogenic stage of the developed lead-zinc deposit.The genesis of the deposit belongs to the medium and low temperature hydrothermal metasomatic lead-zinc deposit controlled by structure+lithofacies.

developed lead-zinc oretrace elementsLA-ICP-MSgenesis of deposit

左家庚、陈恩近

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彝良驰宏矿业有限公司,云南彝良 657600

发达铅锌矿 微量元素 LA-ICP-MS 矿床成因

2024

四川有色金属
四川省有色冶金研究院

四川有色金属

影响因子:0.236
ISSN:1006-4079
年,卷(期):2024.(4)