《Table 1 Whole-rock major and trace element compositions of the iron ore samples (Fe2O3T>30wt%) f
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《"Petrological and Geochemical Constraints on the Protoliths of Serpentine-Magnetite Ores in the Zhaoanzhuang Iron Deposit, Southern North China Craton"》
Fe2O3T，total Fe expressed as Fe2O3；CN，chondrite-normalized.
Whole-rock geochemical analyses were performed at the Analytical Laboratory of Beijing Research Institute of Uranium Geology（ALBRIUG）.Major elements were determined using a Phillips PW2404 X-ray fluorescence spectrometer and chemical analytical method.The analytical error is less than 5%.Conventional wet chemical analyses were used for measuring Fe O content with error of 0.5%.Trace and rare earth elements were determined by inductively coupled plasma mass spectrometer（ICP-MS）using a German Finnigan MAT Element spectrometer HR-ICP-MS.The relative error was less than 5%when the content was>10 ppm，less than10%when<10 ppm.The analytical results are listed in Table 1 and 2.
| 图表编号 | XD0017171100 严禁用于非法目的 |
|---|---|
| 绘制时间 | 2018.04.01 |
| 作者 | MENG Jie、LI Houmin、LI Lixing、SANTOSH M.、SONG Zhe、YANG Xiuqing |
| 绘制单位 | MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences、State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences and Resources, China University o |
| 更多格式 | 高清、无水印（增值服务） |
