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中国新生代上地幔铅同位素地球化学场对成岩、成矿物质来源的制约——以斑岩铜矿床及铜镍硫化物矿床为例

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马振东, 方俊杰, 刘小权. 2019. 中国新生代上地幔铅同位素地球化学场对成岩、成矿物质来源的制约——以斑岩铜矿床及铜镍硫化物矿床为例[J]. 中国地质, 46(1): 32-42. doi: 10.12029/gc20190103
引用本文: 马振东, 方俊杰, 刘小权. 2019. 中国新生代上地幔铅同位素地球化学场对成岩、成矿物质来源的制约——以斑岩铜矿床及铜镍硫化物矿床为例[J]. 中国地质, 46(1): 32-42. doi: 10.12029/gc20190103
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MA Zhendong, FANG Junjie, LIU Xiaoquan. 2019. Constraints of the lead isotope geochemical field of the Upper Mantle in China on diagenetic and ore-forming materials exemplified by porphyry copper deposit and copper-nickel sulfide deposit[J]. Geology in China, 46(1): 32-42. doi: 10.12029/gc20190103
Citation: MA Zhendong, FANG Junjie, LIU Xiaoquan. 2019. Constraints of the lead isotope geochemical field of the Upper Mantle in China on diagenetic and ore-forming materials exemplified by porphyry copper deposit and copper-nickel sulfide deposit[J]. Geology in China, 46(1): 32-42. doi: 10.12029/gc20190103
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中国新生代上地幔铅同位素地球化学场对成岩、成矿物质来源的制约——以斑岩铜矿床及铜镍硫化物矿床为例

  • 中国地质大学(武汉), 湖北 武汉 430074

  • 基金项目:
    中国地质调查局项目“中国地球化学场与成矿关系研究”课题（DD20160346）资助
详细信息
    作者简介: 马振东, 男, 1943年生, 教授, 从事地球化学方向的教学和科研; E-mail:zhdongma@163.com

  • 中图分类号: P594+.1;P618.41

Constraints of the lead isotope geochemical field of the Upper Mantle in China on diagenetic and ore-forming materials exemplified by porphyry copper deposit and copper-nickel sulfide deposit

  • China University of Geosciences(Wuhan), Wuhan 430074, Hubei, China

  • Fund Project: Supported by China Geological Survey Project (No.DD20160346)
More Information
    Author Bio: MA Zhendong, male, born in 1943, professor, majors in the teaching and study of geochemistry; E-mail: zhdongma@163.com .

    摘要

  • 区域成矿带铅稳定同位素地球化学研究是区域地球化学分区、示踪成岩成矿物质来源、阐明矿床成因的有效途径。本文以中国特有的大地构造背景为基础，以新生代上地幔铅同位素组成的地球化学场为依据，示踪了中国大型、超大型斑岩型铜矿床及铜镍硫化物型矿床的成岩成矿物质来源。结果显示：①斑岩型铜矿床及铜镍硫化物型矿床成矿母岩继承了所属陆块的上地幔铅同位素组成特征；②两类矿床的含矿岩体和矿石矿物铅同位素组成十分一致，示踪两者同源；壳熔花岗岩和围岩地层的铅同位素组成与矿石铅同位素组成迥异；③位于各陆块的斑岩型铜矿床及铜镍硫化物型矿床的成矿母岩和矿石铅同位素组成除继承了各陆块上地幔不同的铅同位素组成特征外，还示踪了壳幔层圈间耦合性的“块体效应”，同时，上地幔铅同位素组成可能还具“延迟效应”。

    The lead stable isotope geochemistry of regional metallogenic belts is an effective means for making regional geochemical zoning, tracing diagenetic ore-forming sources, and elucidating the genesis of deposits. Based on the unique tectonic setting of China, the authors have traced the diagenesis of large-sized and superlarge porphyry copper deposits and copper-nickel sulfide deposits in China based on the geochemical field of the lead isotope composition of the upper mantle in China for sources of ore-forming materials. Some conclusions have been reached:1. The porphyry copper deposit and the copper-nickel sulfide type ore-forming parent rock inherit the lead isotope composition of the upper mantle of the adjacent land mass; 2. The lead isotope composition of the ore-bearing rock mass and ore minerals of the two types of deposits is obviously consistent with each other, and the two traces are homologous; the lead isotope composition of the shell fused granite and surrounding strata is different from that of the ore; 3. In addition to inheriting different lead isotope composition characteristics of the mantle on each land mass, the lead isotope composition of rock and ore in the porphyry copper deposits and the copper-nickel sulfide deposits of each land mass also trace the "block effect" of the coupling between the crust and the mantle layers. At the same time, the lead isotope composition of the upper mantle may exhibits "delay effect".

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  • 图 1  中国新生代地幔及斑岩型铜矿和铜镍硫化物矿床206Pb/204Pb铅同位素组成分布(据路凤香2009, 修改)

    Figure 1. 

    下载: 全尺寸图片 幻灯片

    图 2  德兴斑岩铜矿床矿石铅、含铜斑岩体、大茅山岩体铅同位素组成

    Figure 2. 

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    图 3  玉龙斑岩铜矿带含矿岩体全岩铅及矿石铅同位素组成投点图

    Figure 3. 

    下载: 全尺寸图片 幻灯片

    图 4  金川铜镍矿床铅同位素组成投点图

    Figure 4. 

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    图 5  喀拉通克铜镍矿床铅同位素组成投点图

    Figure 5. 

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    表 1  中国大型-超大型斑岩铜矿地质、206Pb/204Pb铅同位素组成特征

    Table 1.  Characteristics of large-superlarge porphyry copper deposits in China, 206Pb/204Pb lead isotope composition

    下载: 导出CSV

    表 2  Ⅰ-⑥隐伏矿体与花岗岩全岩及其附近矿体铅同位素组成

    Table 2.  Lead isotope composition of Ⅰ-6 concealed ore body and granite whole rock and its adjacent ore body

    下载: 导出CSV

    表 3  喀拉通克一号铜镍矿床铅同位素组成

    Table 3.  Lead isotope composition of the Kalatongke No.1 copper-nickel deposit

    下载: 导出CSV
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收稿日期:  2018-11-16
修回日期:  2018-12-12
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