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凤太矿集区东塘子铅锌矿床S、Pb同位素组成对成矿物质来源的示踪

张革利, 田涛, 王瑞廷, 高卫宏, 常宗东. 2020. 凤太矿集区东塘子铅锌矿床S、Pb同位素组成对成矿物质来源的示踪[J]. 中国地质, 47(2): 472-484. doi: 10.12029/gc20200214
引用本文: 张革利, 田涛, 王瑞廷, 高卫宏, 常宗东. 2020. 凤太矿集区东塘子铅锌矿床S、Pb同位素组成对成矿物质来源的示踪[J]. 中国地质, 47(2): 472-484. doi: 10.12029/gc20200214
ZHANG Geli, TIAN Tao, WANG Ruiting, GAO Weihong, CHANG Zongdong. 2020. S, Pb isotopic composition of the Dongtangzi Pb-Zn deposit in the Fengtai ore concentration area of Shaanxi Province for tracing sources of ore-forming materials[J]. Geology in China, 47(2): 472-484. doi: 10.12029/gc20200214
Citation: ZHANG Geli, TIAN Tao, WANG Ruiting, GAO Weihong, CHANG Zongdong. 2020. S, Pb isotopic composition of the Dongtangzi Pb-Zn deposit in the Fengtai ore concentration area of Shaanxi Province for tracing sources of ore-forming materials[J]. Geology in China, 47(2): 472-484. doi: 10.12029/gc20200214

凤太矿集区东塘子铅锌矿床S、Pb同位素组成对成矿物质来源的示踪

  • 基金项目:
    中国地质调查局项目(DD2016005213)和西北有色地矿集团科技项目(XD20190023)资助
详细信息
    作者简介: 张革利, 男, 1971年生, 高级工程师, 主要从事地质勘查工作; E-mail:842073390@qq.com
    通讯作者: 田涛, 男, 1988年生, 硕士, 工程师, 主要从事地球化学与矿产勘查工作; E-mail:tiantao8825@163.com
  • 中图分类号: P632

S, Pb isotopic composition of the Dongtangzi Pb-Zn deposit in the Fengtai ore concentration area of Shaanxi Province for tracing sources of ore-forming materials

  • Fund Project: Supported by China Geological Survey Program (No. DD2016005213) and Science and Technology Project of Northwest Nonferrous Mining Group (No. XD20190023)
More Information
    Author Bio: ZHANG Geli, male, born in 1971, senior engineer, mainly engages in geological exploration; E-mail:842073390@qq.com .
    Corresponding author: TIAN Tao, male, born in 1988, master, senior engineer, majors in the study of geochemistry and geological exploration; E-mail: tiantao8825@163.com
  • 东塘子铅锌矿床是秦岭成矿带中典型的铅锌矿床之一,前人对东塘子铅锌矿床成矿作用研究较多,但受限于测试手段及认识的局限性,多年来对其物质来源的认识仍未统一。本文在充分研究东塘子铅锌矿床地质特征的基础上,开展了相关样品的S、Pb同位素分析,分析对象包括了不同类型的铅锌矿石,讨论了该铅锌矿床的成矿物质来源、区内岩浆岩与铅锌成矿的关系等。研究表明:东塘子铅锌矿床矿石硫化物δ34S值变化范围为1.8‰~12.5‰,平均7.50‰,计算获得成矿流体中总硫δ34S∑S为7.7‰,显示海水硫酸盐(蒸发膏岩)与岩浆硫的混合来源特征。矿石铅同位素组成稳定,铅源主要来自富U-Th-Pb的上地壳与深部,可能与深部岩浆活动有关。研究结果表明,东塘子铅锌矿床的成矿过程与南秦岭印支期大规模多阶段构造-岩浆-流体活动密切相关,为下一阶段区内找矿工作提供了新的思路。

  • 加载中
  • 图 1  凤太矿集区西部矿产地质简图

    Figure 1. 

    图 2  东塘子铅锌矿床地质简图(a)与联合剖面图(b)

    Figure 2. 

    图 3  东塘子铅锌矿床矿石及矿相显微照片

    Figure 3. 

    图 4  东塘子铅锌矿床矿石硫同位素组成频率直方图(a)与总硫同位素组成(b)

    Figure 4. 

    图 5  不同来源S同位素特征图

    Figure 5. 

    图 6  东塘子铅锌矿床矿石铅同位素模式图(底图据Doe and Zartman, 1979)

    Figure 6. 

    图 7  东塘子铅锌矿床矿石铅△β-△γ成因判别图解(据朱炳泉等,1998

    Figure 7. 

    表 1  东塘子铅锌矿床硫同位素组成

    Table 1.  Sulfur isotope composition of the Dongtangzi Pb−Zn deposit

    下载: 导出CSV

    表 2  东塘子铅锌矿床铅同位素组成

    Table 2.  Pb isotopic composition of the Dongtangzi Pb−Zn deposit

    下载: 导出CSV

    表 3  东塘子铅锌矿床与洞中拉、栖霞山铅锌矿床特征对比

    Table 3.  The comparison between Dongtangzi, Dongzhongla and Xixiashan deposits

    下载: 导出CSV
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出版历程
收稿日期:  2018-07-24
修回日期:  2018-11-30
刊出日期:  2020-04-25

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