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    地壳性质对滇西南锡矿床分布的约束: 基于Hf同位素填图

    裴桐 孙祥 郑明俊 苗珂 梁晓雅

    裴桐, 孙祥, 郑明俊, 苗珂, 梁晓雅, 2025. 地壳性质对滇西南锡矿床分布的约束: 基于Hf同位素填图. 地球科学, 50(11): 4229-4242. doi: 10.3799/dqkx.2024.133
    引用本文: 裴桐, 孙祥, 郑明俊, 苗珂, 梁晓雅, 2025. 地壳性质对滇西南锡矿床分布的约束: 基于Hf同位素填图. 地球科学, 50(11): 4229-4242. doi: 10.3799/dqkx.2024.133
    Pei Tong, Sun Xiang, Zheng Mingjun, Miao Ke, Liang Xiaoya, 2025. Nature of Crust Constraints on Tin Deposit Distribution in Southwest Yunnan: Based on Hf Isotope Mapping. Earth Science, 50(11): 4229-4242. doi: 10.3799/dqkx.2024.133
    Citation: Pei Tong, Sun Xiang, Zheng Mingjun, Miao Ke, Liang Xiaoya, 2025. Nature of Crust Constraints on Tin Deposit Distribution in Southwest Yunnan: Based on Hf Isotope Mapping. Earth Science, 50(11): 4229-4242. doi: 10.3799/dqkx.2024.133

    地壳性质对滇西南锡矿床分布的约束: 基于Hf同位素填图

    doi: 10.3799/dqkx.2024.133
    基金项目: 

    国家自然科学基金重大研发计划重点支持项目 92162215

    高等学校学科创新引智计划项目 BP0719021

    详细信息
      作者简介:

      裴桐(2001-),男,硕士研究生,主要从事与花岗岩有关的铜锡成矿作用研究. ORCID:0009-0001-0005-7627. E-mail:pei_t@qq.com

      通讯作者:

      孙祥, E-mail: sunxiang@cugb.edu.cn

    • 中图分类号: P597;P618

    Nature of Crust Constraints on Tin Deposit Distribution in Southwest Yunnan: Based on Hf Isotope Mapping

    • 摘要:

      滇西南锡矿带是我国重要的锡成矿带之一,前人总结了滇西南锡矿带中与花岗岩相关的锡矿床的时空分布,但对锡矿床的空间展布情况与地壳性质的关系以及其控制锡成矿的原因尚不清楚.本文收集了滇西南地区已发表的早古生代‒新生代花岗岩类的锆石Hf同位素数据,在前人对三江特提斯造山带大范围同位素填图的基础上,利用ArcGIS软件绘制了滇西南地区锆石εHft)值和TDMC等值线图及两条典型剖面图.成图结果表明,昌宁‒孟连造山带和保山地体表现为低εHft)高TDMC的古老地壳特征,而腾冲地体同位素分布不均匀,既存在低εHft)高TDMC的古老地壳区,又存在高εHft)低TDMC的新生地壳区.滇西南地区的锡矿分布与地壳性质关系密切,锡矿均分布于低εHft)高TDMC的古老地壳区,而在高εHft)低TDMC的新生地壳区,尚未发现锡矿.锡矿在古老地壳区域的集中产出可能与古老富锡地壳有关.贫锡且高氧逸度地幔岩浆的混入对花岗岩中锡的富集具有抑制作用,可能是新生地壳区锡成矿作用不明显的原因.

       

    • 图  1  东南亚地质简图(a.据Metcalfe, 2021修改)和滇西南花岗岩与锡矿床分布简图(b.据Zhao et al., 2017; Wang et al., 2021; 孙祥等, 2023修改)

      Fig.  1.  Tectonic sketch map of Southeast Asia (a. modified after Metcalfe, 2021) and distribution diagram of granite and tin deposits in the Southwest Yunnan (b. modified after Zhao et al., 2017; Wang et al., 2021; Sun et al., 2023)

      图  2  滇西南花岗岩锆石εHf(t)与U-Pb年龄

      Fig.  2.  Plots of εHf(t) versus U-Pb ages of granite zircons in Southwest Yunnan

      图  3  滇西南花岗岩锆石εHf(t)等值线图

      Fig.  3.  Zircon εHf(t) contour map of granites in Southwest Yunnan

      图  4  滇西南花岗岩锆石TDMC等值线图

      Fig.  4.  Zircon TDMC contour map of granites in Southwest Yunnan

      图  5  锆石εHf(t)值和TDMC沿A-A’和B-B’剖面的变化

      Fig.  5.  Variations in zircon εHf(t) and TDMC values along A-A′ and B-B′ profiles

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