铅锌矿床中闪锌矿Cd含量及Zn/Cd值的地质意义

王光辉, 刘兵, 匡爱兵. 铅锌矿床中闪锌矿Cd含量及Zn/Cd值的地质意义[J]. 西北地质, 2016, 49(3): 132-140.
引用本文: 王光辉, 刘兵, 匡爱兵. 铅锌矿床中闪锌矿Cd含量及Zn/Cd值的地质意义[J]. 西北地质, 2016, 49(3): 132-140.
WANG Guanghui, LIU Bing, KUANG Aibing. Cd contents and Zn/Cd Ratios of Sphalerites and Their Geological Implications[J]. Northwestern Geology, 2016, 49(3): 132-140.
Citation: WANG Guanghui, LIU Bing, KUANG Aibing. Cd contents and Zn/Cd Ratios of Sphalerites and Their Geological Implications[J]. Northwestern Geology, 2016, 49(3): 132-140.

铅锌矿床中闪锌矿Cd含量及Zn/Cd值的地质意义

  • 基金项目: 中国科学院地球化学研究所“Cd同位素对铅锌矿床的地球化学示踪研究——以川滇黔低温成矿域为例”(41503011)

Cd contents and Zn/Cd Ratios of Sphalerites and Their Geological Implications

  • 以5个典型铅锌矿床为研究对象,测试了其闪锌矿中的Zn和Cd含量,发现同一标本上深色闪锌矿比晚期的浅色闪锌矿更富集Cd,其原因可能与流体中Zn/Cd值变化相关;而对比不同矿床不同颜色闪锌矿之间Cd的富集规律是没有意义的。同时,与岩浆作用相关的铅锌矿床,其闪锌矿中的Zn/Cd值与相关岩浆岩的Zn/Cd值相似,暗示闪锌矿中的Zn/Cd值可指示成矿物质来源。同时,川滇黔地区铅锌矿床显示出2组不同的Zn/Cd值:①高Zn/Cd值型(300~800),以会泽矿床为代表,其Zn/Cd值介于峨眉山玄武岩和该区地层之间,暗示该类型矿床的成矿物质可能主要来源于峨眉山玄武岩和地层。②低Zn/Cd值型(20~70),以富乐矿床为代表,其Zn/Cd值基本与地层相似,暗示该矿床的成矿物质可能主要来源于地层。而对比川滇黔地区铅锌矿床和与岩浆作用相关矿床的Cd含量及Zn/C值发现,成因不同的矿床,其Cd含量和Zn/Cd值具有较大差异。因此,铅锌矿床闪锌矿中的Cd含量及Zn/Cd值对于判别成矿物质来源和矿床成因具有指示意义。
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出版历程
收稿日期:  2016-01-06
修回日期:  2016-05-25
刊出日期:  2016-09-15

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