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有色金属(矿山部分):2019,71(6):49-58
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广东天堂山锡多金属矿床地质及硫同位素特征
(1.(1. 中国地质大学(北京),北京 100083;2. 中国地质调查局发展研究中心,北京 100037;3. 中国地质调查局,北京 100037))
Geological and sulfur isotope characteristics of Tiandushan Tin Polymetallic Deposit in Guangdong province
(1.(1. China University of Geosciences, Beijing 100083, China;2. Development and Research Centre, China Geological Survey, Beijing 100037, China;3. China Geological Survey, Beijing 100037, China))
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中文摘要: 天堂山锡多金属矿位于南岭成矿带的东段,河源深断裂带与大东山—浰源—罗浮东西向深断裂带交汇处附近,中生代大长沙火山岩盆地中南部边缘。在分析该矿床成矿地质条件的基础上,系统研究了矿石硫同位素组成特征,其结果表明矿石硫化物的硫同位素组成变化范围较窄,成矿热液δ34SΣS在3.0‰附近,反映其来源与岩浆硫密切相关。
Abstract:The Tiantangshan tin polymetallic deposit is located in the eastern part of the Nanling metallogenic belt, near the junction of the Heyuan deep fault zone and the Dadongshan-Wuyuan-Luofu east-west deep fault zone, and the middle and southern margin of the Mesozoic Dachangsha volcanic rock basin. Based on the analysis of the ore-forming geological conditions of the deposit, the characteristics of sulfur isotopic composition of the ore were systematically studied. The results indicated that the sulfur isotope composition of ore sulfides had a narrow range of variation, and the ore-forming hydrothermal fluid δ34SΣS was around 3.0‰, reflecting that its source closely related to magma sulfur.
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基金项目:老矿山找矿技术创新与示范项目(1212011220737),矿集区矿产调查及深部找矿预测(DD20190570)
引用文本:
张志辉1,2,贾宏翔1,胡擘捷1,耿 林3,贾儒雅2.广东天堂山锡多金属矿床地质及硫同位素特征[J].有色金属(矿山部分),2019,71(6):49-58.
ZHANG Zhihui1,2,JIA Hongxiang1,HU Bojie1,GENG Lin3,JIA Ruya2.Geological and sulfur isotope characteristics of Tiandushan Tin Polymetallic Deposit in Guangdong province[J].NONFERROUS METALS(Mining Section),2019,71(6):49-58.

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