| 豫西熊耳山矿集区栾灵金矿床辉钼矿Re-Os同位素年龄及其地质意义 |
| Received:June 14, 2015 Revised:November 26, 2015 点此下载全文 |
| 引用本文：CHAO WeiWei,YE HuiShou,TIAN Ye,LIU YanMing,LU DongYu,WA NG Peng,JIAN Wei,ZHANG XingKang.2016.Re-Os isotopic dating of molybdenite from Luanling gold deposit in Xiong'er Mo untain ore concentration area of western Henan Province and its geological sig nificance[J].Mineral Deposits,35(1):103~116 |
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| Author Name | Affiliation | E-mail | | CHAO WeiWei | School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China | weiweichao@cugb.edu.cn | | YE HuiShou | MRL Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, CAGS, Beijing 100037, China | yehuishou@163.com | | TIAN Ye | Luanling Gold Deposit Corpora-tion of Luanchuan County,Luanchuan 471500, Henan , China | | | LIU YanMing | Luanling Gold Deposit Corpora-tion of Luanchuan County,Luanchuan 471500, Henan , China | | | LU DongYu | School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China | | | WA NG Peng | School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China | | | JIAN Wei | MRL Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, CAGS, Beijing 100037, China | | | ZHANG XingKang | School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China | |
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| 基金项目:本文得到国家自然科学基金项目(编号: 41272104、41573036)和地质调查项目(编号: 12120114035401、1212011220869)联合资助 |
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| 中文摘要:豫西栾灵金矿床地处熊耳山金多金属矿集区南部马超营断裂带北侧, 金矿体产 于构造破碎带中,呈钾长石石英脉体和蚀变岩产出,为本区一种新的金矿化类型。文章为厘 定栾灵金矿床的成矿时代,采用辉钼矿Re-Os同位素定年方法,测得栾灵金矿6 件辉钼矿样 品的Re-Os同位素模式年龄为(161±3) Ma～(164±2) Ma,加权平均年龄(163±1) Ma (MSWD=068),等时线年龄 (163 ± 2) Ma(MSWD = 15),表明栾灵金矿床 形成于晚侏罗世早期。与祁雨沟、前河金矿等早白垩世(125 Ma)金矿相比,栾灵金矿的成 矿作用早约38 Ma。这些年龄数据表明,该矿床在区域上可能与南泥湖-三道庄、上房沟钼矿 等形成于同一成矿系统,它的发现为在熊耳山地区寻找相似成矿地质条件的金、钼矿床提供 了依据。 |
| 中文关键词:地球化学 矿床特征 辉钼矿 Re-Os同位素年龄 栾灵金矿床 豫西 |
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| Re-Os isotopic dating of molybdenite from Luanling gold deposit in Xiong'er Mo untain ore concentration area of western Henan Province and its geological sig nificance |
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| Abstract:The Luanling gold deposit is located on the northern side of Machaoying fault zo ne in the southern part of the Xiong’er Mountain gold polymetallic ore district ,Henan Province. The gold orebodies mainly occur as the K-feldspar-quartz vein or altered rock in the structural fracture zone. For the purpose of studying the chronology of the gold mineralization in the Luanling gold deposit,the authors purified molybdenite from the gold-bearing feldspar quartz veins in the Luanlin g gold deposit. Re-Os dating of these minerals yielded modal ages from (161±3 ) Ma to (164±2) Ma, a weighted average age of (163±1) Ma(MSWD=068), and an isochron age of (163±2) Ma(MSWD=15), implying that the Luanling g old deposit formed in the Late-Jurassic. Compared with the Cretaceous(125 Ma) Qiyugou gold deposit and Qianhe gold deposit, the Luanling gold depos it formed about 38 Ma earlier, indicating a new late Jurassic mineralization pe riod in the Xiong’er ore concentration area. The Luanling gold deposit and Nann ihu-Sandaozhuang as well as Shangfanggou Mo deposits were produced by the same m ineralization system. The discovery of the Luanling Au deposit provides the basi s for the study of Au-Mo deposits of the similar ore-forming conditions in the X iong'er Mountain region. |
| keywords:geochemistry, deposit characteristics, molybdenite, Re-Os isotopic age, Luanling gold deposit, western Henan |
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