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Development of CA-ID-TIMS zircon U–Pb dating technique at Guangzhou Institute of Geochemistry, Chinese Academy of Sciences

机译:中国科学院广州地球化学研究所开发CA-ID-TIMS锆石U-Pb测年技术

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U–Pb geochronology using isotope dilution-thermal ionization mass spectrometry (ID-TIMS) is by far the most precise analytical technique. It affords the opportunity to determine 206Pb/238U dates with unprecedented precision often <1‰ on single analyses or weighted mean dates derived from multiple analyses. Pretreatment protocols for zircon analysis, and community-wide innovations spurred on by EARTHTIME tends to be at the leading edge of technological development. Also, more and more Chinese researchers perform lots of laboratory work in improving the technique in China. Here we present the running condition, procedural blanks and zircon standards measurement results in the clean laboratory of the Guangzhou Institute of Geochemistry, Chinese Academy of Sciences (GIGCAS). The results show the total procedural blanks (Pbc) are below ~1?pg mostly, suitable for the sample pretreatment and operation. The 206Pb/238U dates of R33 and 500?Ma solution are 419.88?±?0.94?Ma (n?=?7; MSWD?=?6.8) and 500.50?±?0.19?Ma (n?=?9; MSWD?=?0.84), respectively. These results demonstrate that the CA-ID-TIMS procedure is well established at GIGCAS. Our efforts are beneficial to the development of EARTHTIME-CN program. In particular, when this technique is combined with the SIMS technique, it provides an efficient way to solve a number of geochronological problems encountered in China and worldwide.
机译:迄今为止,使用同位素稀释-热电离质谱法(ID-TIMS)进行的U–Pb地球年代学是最精确的分析技术。它提供了机会以前所未有的精度确定206Pb / 238U日期,这些精度通常在单次分析中或从多次分析中得出的加权平均日期通常<1‰。锆石分析的预处理方案以及EARTHTIME推动的社区范围内的创新往往处于技术发展的前沿。而且,越来越多的中国研究人员在改进中国技术方面进行了大量的实验室工作。在这里,我们介绍了中国科学院广州地球化学研究所洁净实验室的运行状况,程序空白和锆石标准测量结果。结果表明,程序空白总量(Pbc)大多在〜1µpg以下,适合样品的前处理和操作。 R33和500?Ma溶液的206Pb / 238U日期为419.88?±?0.94?Ma(n?=?7; MSWD?=?6.8)和500.50?±?0.19?Ma(n?=?9; MSWD? =?0.84)。这些结果表明,CA-ID-TIMS程序已在GIGCAS上确立。我们的努力有利于EARTHTIME-CN计划的发展。特别是,当该技术与SIMS技术结合使用时,它提供了一种有效的方法来解决中国和世界范围内遇到的许多地质年代问题。

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