| 大别山南麓梨木岭钼矿床辉钼矿Re-Os同位素年龄及地质意义 |
| Received:May 08, 2016 Revised:June 19, 2017 点此下载全文 |
| 引用本文：GONG YinJie,ZHU Jiang,CHEN DongMing,ZHANG ZunZun,FAN Chuan.2017.Re-Os isotopic ages of Limuling molybdenum deposit in southern Dabie Mountain and their geological significance[J].Mineral Deposits,36(4):992~1002 |
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| Author Name | Affiliation | | GONG YinJie | Wuhan Center of China Geological Survey, Wuhan 430205, Hubei, China
Research Center of Granitic Diagenesis and Mineralization, China Geological Survey, Wuhan 430205, Hubei, China | | ZHU Jiang | Wuhan Center of China Geological Survey, Wuhan 430205, Hubei, China
Research Center of Granitic Diagenesis and Mineralization, China Geological Survey, Wuhan 430205, Hubei, China | | CHEN DongMing | Hubei Geological Survey, Wuhan 430034, Hubei, China | | ZHANG ZunZun | Wuhan Center of China Geological Survey, Wuhan 430205, Hubei, China
Research Center of Granitic Diagenesis and Mineralization, China Geological Survey, Wuhan 430205, Hubei, China | | FAN Chuan | Hubei Geological Survey, Wuhan 430034, Hubei, China |
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| 基金项目:本文为中国地质调查局地质大调查项目（编号：DD20179232）和（编号：1212011220515）联合资助的成果 |
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| 中文摘要:梨木岭钼矿床是近年来新发现的钼矿，也是目前大别山构造带唯一具有工业意义的中型钼矿床。通过辉钼矿Re-Os同位素年代学测定，获得梨木岭钼矿Ⅰ矿脉5件样品辉钼矿的Re-Os模式年龄为（115.3±1.4） Ma~（118.1±1.5） Ma，加权平均年龄为（116.8±1.3） Ma；等时线年龄为（119.9±6.2） Ma（MSWD=1.6）。Ⅱ矿脉2件辉钼矿Re-Os模式年龄分别为（114.7±1.6） Ma和（117.0±1.4） Ma。两条矿脉中辉钼矿样品的Re-Os模式年龄在误差范围内一致，表明这两条矿脉为早白垩世同期热液产物。梨木岭钼矿床可能为与早白垩世中酸性岩浆活动有关的岩浆热液型矿床。早白垩世大别山钼成矿作用不仅仅局限在北大别的北淮阳构造带，在大别山南麓同样存在该阶段钼成矿作用。 |
| 中文关键词:地球化学 辉钼矿Re-Os同位素测年 早白垩世 钼成矿作用 梨木岭钼矿 大别山南麓 |
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| Re-Os isotopic ages of Limuling molybdenum deposit in southern Dabie Mountain and their geological significance |
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| Abstract:The Limuling molybdenum deposit in southern Dabie area consists of quartz-sulfide veins. Re-Os dating of five molybdenite samples in No.Ⅰ orebody yielded model ages ranging from (115.3±1.4) Ma to(118.6±1.5) Ma, with an average of (116.8±1.3) Ma. Two molybdenite samples in No. Ⅱ orebody yielded model ages of (114.7±1.6) Ma and (117.0±1.4) Ma, respectively. The Re-Os ages of the two ore bodies are identical within the error, suggesting that they were formed in the Early Cretaceous. These new data, combined with geochronological results available from the other molybdenum deposits in northern Huaiyang region, imply that magmatism and Mo mineralization occurred in the Tongbai-Dabie belt during the Early Cretaceous. |
| keywords:geochemistry Re-Os molybdenite dating Early Cretaceous molybdenum mineralization Limuling molybdenum deposit Dabie Mountain area |
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