首页> 外文期刊>Journal of Asian earth sciences >In situ rutile U-Pb dating based on zircon calibration using LA-ICP-MS, geological applications in the Dabie orogen, China
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In situ rutile U-Pb dating based on zircon calibration using LA-ICP-MS, geological applications in the Dabie orogen, China

机译:基于LA-ICP-MS的锆石标定的原位金红石型U-Pb定年,中国大别造山带的地质应用

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Rutile U-Pb dating by laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) has received increasing attention in geological applications. Previous natural rutile reference materials are insufficient to meet the growing demand of working standards for laser U/Pb dating. In present study, we have developed a new calibration strategy for LA-ICP-MS rutile dating using the most popular zircon as reference material. The matrix-dependent elemental fractionation of rutile and zircon could effectively decrease to a better level by optimized analytical parameters and with large ablation spot size (44-90 mu m). The acceptable Pb/U correction coefficient between rutile and zircon could be obtained while the diameter/depth ratio of the crater is above 1 after assessing elemental fractionation of different ablation size. Five rutile were analyzed by zircon calibration, and their ages show strong agreement with those obtained by secondary ion mass spectrometry (SIMS) or thermal ionization mass spectrometry (TIMS) analysis, with both precision and accuracy within +/- 2%. Two rutiles of eclogitic rocks from the Dabie orogen yield the ages of 207.0 +/- 2.1 Ma and 205.6 +/- 2.4 Ma, respectively. Both ages are conceivably younger than that previously reported rutile ages (218 Ma) for eclogites. The quite different U-Pb ages of rutile from different localities most likely indicate the different exhumation history of the subducted continental crust. LA-ICP-MS rutile U-Pb dating using zircon as an external calibration reference material would assuage rutile reference material insufficient supply and improve its widespread application.
机译:通过激光烧蚀电感耦合等离子体质谱法(LA-ICP-MS)进行金红石型U-Pb定年在地质应用中越来越受到关注。以前的天然金红石标准物质不足以满足激光U / Pb测年的工作标准不断增长的需求。在本研究中,我们使用最受欢迎的锆石作为参考材料,为LA-ICP-MS金红石测年开发了一种新的校准策略。金红石和锆石的基质相关元素分馏可通过优化分析参数并具有较大的烧蚀斑尺寸(44-90微米)有效降低至更好的水平。在评估不同烧蚀尺寸的元素分数后,当陨石坑的直径/深度比大于1时,可以获得金红石和锆石之间可接受的Pb / U校正系数。通过锆石校准分析了五种金红石,它们的年龄与通过二次离子质谱(SIMS)或热电离质谱(TIMS)分析获得的金红石具有高度一致性,其准确性和准确性均在+/- 2%之内。来自大别造山带的两片金红石岩石年龄分别为207.0 +/- 2.1 Ma和205.6 +/- 2.4 Ma。可以想象,这两个年龄都比以前报道的榴辉岩的金红石年龄(218 Ma)年轻。来自不同地区的金红石的U-Pb年龄完全不同,很可能表明俯冲大陆壳的发掘历史不同。使用锆石作为外部校准参考材料的LA-ICP-MS金红石U-Pb定年法可以缓解金红石参考材料的供应不足并改善其广泛应用。

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