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| 华南下寒武统Ni-Mo-Se多金属层S-Se同位素体系 | |
| 引用本文： | 樊海峰,温汉捷,张羽旭,朱传威,黄晶,储雪蕾.华南下寒武统Ni-Mo-Se多金属层S-Se同位素体系[J].地学前缘,2012,19(4):266-275. |
| 作者姓名： | 樊海峰 温汉捷 张羽旭 朱传威 黄晶 储雪蕾 |
| 作者单位： | 1. 矿床地球化学国家重点实验室,中国科学院地球化学研究所,贵州贵阳550002 2. 矿床地球化学国家重点实验室,中国科学院地球化学研究所,贵州贵阳550002 中国科学院研究生院,北京100039 3. 岩石圈演化国家重点实验室,中国科学院地质与地球物理研究所,北京100029 |
| 基金项目： | 国家自然科学基金项目，贵州省自然科学基金项目，国家科技部专项(KCZX20100104) 感谢中国科学院地球化学研究所环境国家重点实验室安宁老师分析硫同位素;匿名审稿人对本文提出了建设性意见;在此也表示感谢 |
| 摘 要： | 为了进一步理解华南下寒武统Ni-Mo-Se多金属层的物质来源及形成环境,文中分析了遵义中南村和张家界后坪两个Ni-Mo-Se矿层及其围岩的黄铁矿硫同位素和全岩的硒同位素组成。硫同位素组成显示两个Ni-Mo-Se矿层形成时的环境存在区域性差别,中南村矿层形成于间歇开放的海洋环境,而后坪矿层形成于封闭的缺氧(静海)环境。较大的硫同位素范围暗示硫酸盐还原菌控制硫同位素的分馏,而热液流体可能提供了大量金属元素,从而导致矿层富集大量的硫化物和稀有金属。硒同位素组成指示牛蹄塘组底部热液流体的Se可能重新经历了氧化还原循环,而Se的富集过程可能受有机质和粘土矿物吸附或类质同象过程控制。因此,控制多金属富集的因素主要为富集金属的热液流体的参与和缺氧环境下的自生沉积。 |
| 关 键 词： | 下寒武统 Ni-Mo-Se多金属层 物质来源及形成环境 硫-硒同位素 |
The S and Se isotope of Lower Cambrian Ni-Mo-Se polymetallic layer in South China |
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| Fan Haifeng,Wen Hanjie,Zhang Yuxu,Zhu Chuanwei,Huang Jing,Chu Xuelei.The S and Se isotope of Lower Cambrian Ni-Mo-Se polymetallic layer in South China[J].Earth Science Frontiers,2012,19(4):266-275. | |
| Authors: | Fan Haifeng Wen Hanjie Zhang Yuxu Zhu Chuanwei Huang Jing Chu Xuelei |
| Institution: | 1.State Key Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550002,China 2.State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 3.Graduate University of Chinese Academy of Sciences,Beijing 100039,China |
| Abstract: | Sulfur and selenium isotopic composition of two Ni-Mo-Se ore layers from Zunyi and Zhangjiajie were analyzed to understand the oceanic environment and origin of these Lower Cambrian polymetallic layers in South China.Sulfur isotopic difference suggests that there are different environments for these two ore layers.Ni-Mo-Se ore layer of Zunyi was formed under the environment of open ocean in which sulfate was intermittently inputted,and that of Zhangjiajie formed under more depleted oxygen closed environment.Large scale variation of sulfur isotope indicates that bacterial reduction of sulfate played an important role in the formation of these polymetallic layers.Hydrothermal venting into tectonically formed depressions may provide metals that precipitated with bacterially reduced sulfide.Selenium isotopic composition indicates that Se(-II) derived from hydrothermal fluids could have undergone oxidation-reduction recycling at the bottom host black shales and carbonaceous cherts.The parts of Se enriched in Ni-Mo-Se ore layers were controlled by adsorption of organism and clay minerals and isomorphism processes.In a word,metal-rich hydrothermal fluids and their precipitation under anoxic condition control the the enrichment of metals in Ni-Mo-Se polymetallic layers. |
| Keywords: | Lower Cambrian Ni-Mo-Se polymetallic layers oceanic environment and origin sulfur and selenium isotope |
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