《Table 2 The rang and average of element contents》
本系列图表出处文件名:随高清版一同展现
《A Multi–fluid Constrain for the Forming of Potash Deposits in the Savannakhet Basin: Geochemical Evidence from Halite》
Boron isotopes were measured at the Qinghai Institute of Salt Lakes,Chinese Academy of Sciences(Table 1).Determination of 11B/10B ratios(δ11B)required the samples to be purified prior to analysis;as such,halite was dissolved in solution and then diluted with low-boron water(p H=6–7).These diluted solutions were passed through an Amberlite resin column at a flow rate of 2.5ml/min.Boron was then eluted from the resin using 12 ml of 0.1 mol/L HCl.The eluent was evaporated and dried at60°C,passed through another Amberlite resin column to remove unwanted ions,and then further purified using a low–boron eluent that contained equimolar amounts of mannitol and cesium carbonate(Cs2CO3).Finally,the diluted eluents were evaporated and dried at 60°C,and then prepared for isotopic analysis.
图表编号 | XD0017173300 严禁用于非法目的 |
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绘制时间 | 2018.04.01 |
作者 | REN Qianhui、DU Yongsheng、GAO Donglin、LI Binkai、ZHANG Xiying、LIU Xiuting、YUAN Xiaolong |
绘制单位 | Qinghai Institute of Salt Lakes, Chinese Academy of Sciences、Qinghai Provincial Key Laboratory for Geology and Environment of Salt Lake、University of Chinese Academy of Sciences、Qinghai Institute of Salt Lakes, Chinese Academy of Sciences、Qinghai Provinci |
更多格式 | 高清、无水印(增值服务) |