Robust Timing Constraints for Granitic Magmatism and Hydrothermal Mineralization in the Tieshanlong W-Sn Ore Field, Eastern Nanling Range, South China

IF 3.5 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Wei LI, Juxing TANG, Na GUO, Xinghai LANG, Shiwei SONG, Zhongru WU, Linlin PENG, Xiang FANG, Binfeng CHEN, Dunmei LIAN, Jie LU
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Abstract

The Tieshanlong ore field is an important part of the Nanling Range, which is famous worldwide for its W-Sn mineralization. Notably, the mineralization age of the Tieshanlong ore field is not well constrained, and our field investigation reveals that granitic emplacement occurred at different stages. However, previous studies have not distinguished these multiple stages of magmatism. The Tieshanlong granite complex is closely related to the Huangsha quartz vein-type W-Sn deposit and Tongling skarn-type Cu-W-Sn deposit in this field. Through field investigations and isotopic age analyses, this work studies the relationship between multistage magmatic activity and mineralization in the Tieshanlong ore field. LA-ICP-MS zircon U-Pb isotope analyses revealed that the first- and second-staged granites formed at 154.2 ± 0.6 Ma (MSDW = 1.4) and 151.2 ± 0.4 Ma (MSDW = 1.5), with zircon εHf(t) values ranging from -13.1 to -10.5 and from -14.7 to -11.1, respectively. These data suggest that the Tieshanlong granite complex was derived from the partial melting of ancient crustal material. LA-ICP-MS U-Pb dating of wolframite and cassiterite reveals that W-Sn mineralization occurred at 160–150 Ma, which agrees well with the U-Pb dating results of the second-staged granite within analytical errors. The magmatic activity in this ore field can be divided into three stages: 175–154 Ma, 154–150 Ma and 150–145 Ma. The quartz vein- and skarn-type W-Sn mineralization is closely related to second-staged fine-grained two-mica granite, and formed earlier than skarn-type Cu- mineralization. This study establishes a metallogenic model for the Tieshanlong ore field, and this model has important practical significance for identifying concealed W-Sn(-Cu) deposits around other granitic complexes in the Nanling Range.

Abstract Image

中国南方南岭东部铁山龙钨硒矿田花岗岩岩浆作用和热液成矿作用的时间约束
铁山龙矿田是南岭山脉的重要组成部分,其钨锰矿化闻名于世。值得注意的是,铁山龙矿田的成矿时代尚未得到很好的确定,我们的实地调查显示,花岗岩的成矿作用发生在不同的阶段。然而,以往的研究并没有区分这些不同阶段的岩浆活动。铁山龙花岗岩群与该矿田的黄沙石英脉型钨锡矿床和铜陵矽卡岩型铜锡矿床密切相关。本研究通过野外调查和同位素年龄分析,研究了铁山龙矿区多期岩浆活动与成矿作用之间的关系。LA-ICP-MS锆石U-Pb同位素分析表明,第一期和第二期花岗岩分别形成于154.2 ± 0.6 Ma(MSDW = 1.4)和151.2 ± 0.4 Ma(MSDW = 1.5),锆石εHf(t)值分别为-13.1至-10.5和-14.7至-11.1。这些数据表明,铁山龙花岗岩群是由远古地壳物质部分熔融而成。黑钨矿和锡石的 LA-ICP-MS U-Pb 测定结果表明,W-Sn 矿化发生在 160-150 Ma,与二期花岗岩的 U-Pb 测定结果吻合,误差在分析范围之内。该矿田的岩浆活动可分为三个阶段:175-154 Ma、154-150 Ma 和 150-145 Ma。石英脉和矽卡岩型 W-Sn 矿化与第二期细粒双云母花岗岩密切相关,形成时间早于矽卡岩型铜矿化。该研究建立了铁山龙矿田的成矿模式,对南岭山脉其他花岗岩群周边隐伏钨锡(铜)矿床的识别具有重要的现实意义。
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来源期刊
Acta Geologica Sinica ‐ English Edition
Acta Geologica Sinica ‐ English Edition 地学-地球科学综合
CiteScore
3.00
自引率
12.10%
发文量
3039
审稿时长
6 months
期刊介绍: Acta Geologica Sinica mainly reports the latest and most important achievements in the theoretical and basic research in geological sciences, together with new technologies, in China. Papers published involve various aspects of research concerning geosciences and related disciplines, such as stratigraphy, palaeontology, origin and history of the Earth, structural geology, tectonics, mineralogy, petrology, geochemistry, geophysics, geology of mineral deposits, hydrogeology, engineering geology, environmental geology, regional geology and new theories and technologies of geological exploration.
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