Stepwise chemical abrasion–isotope dilution–thermal ionization mass spectrometry with trace element analysis of microfractured Hadean zircon

IF 2.7 Q2 GEOCHEMISTRY & GEOPHYSICS
C. Brenhin Keller, P. Boehnke, B. Schoene, T. M. Harrison
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引用次数: 4

Abstract

Abstract. The Hadean Jack Hills zircons represent the oldest known terrestrial material, providing a unique and truly direct record of Hadean Earth history. This zircon population has been extensively studied via high-spatial-resolution high-throughput in situ isotopic and elemental analysis techniques, such as secondary ionization mass spectrometry (SIMS), but not by comparatively destructive, high-temporal-precision (<0.05 % two-sigma) thermal ionization mass spectrometry (TIMS). In order to better understand the lead loss and alteration history of terrestrial Hadean zircons, we conduct stepwise chemical abrasion–isotope dilution–thermal ionization mass spectrometry with trace element analysis (CA-ID-TIMS-TEA) on manually microfractured Hadean Jack Hills zircon fragments previously dated by SIMS. We conducted three successive HF leaching steps on each individual zircon fragment, followed by column chromatography to isolate U–Pb and trace element fractions. Following isotopic and elemental analysis, the result is an independent age and trace element composition for each leachate of each zircon fragment. We observe ∼50 Myr of age heterogeneity in concordant residues from a single zircon grain, along with a protracted history of post-Hadean Pb loss with at least two modes circa ∼0 and 2–4 Ga. Meanwhile, stepwise leachate trace element chemistry reveals enrichments of light rare earth elements, uranium, thorium, and radiogenic lead in early leached domains relative to the zircon residue. In addition to confirming the efficacy of the LREE-I alteration index and providing new insight into the mechanism of chemical abrasion, the interpretation and reconciliation of these results suggest that Pb loss is largely driven by low-temperature aqueous recrystallization and that regional thermal events may act to halt – not initiate – Pb loss from metamict domains in the Hadean Jack Hills zircons.
化学磨损-同位素稀释-热电离质谱法分析微断裂冥古宙锆石微量元素
摘要冥古宙杰克山的锆石代表了已知最古老的陆地物质,为冥古宙地球历史提供了独特而真实的直接记录。该锆石种群已通过高空间分辨率、高通量的原位同位素和元素分析技术(如二次电离质谱法(SIMS))进行了广泛的研究,但没有采用相对破坏性的、高时间精度(<0.05 % two-sigma)的热电离质谱法(TIMS)。为了更好地了解陆生冥古宙锆石的铅损失和蚀变历史,我们对SIMS测定的人工微破碎的冥古宙杰克山锆石碎片进行了化学磨损-同位素稀释-热电离质谱联用痕量元素分析(CA-ID-TIMS-TEA)。我们对每个锆石碎片进行了三个连续的HF浸出步骤,然后用柱层析法分离U-Pb和微量元素。通过同位素和元素分析,得出了每个锆石碎片的每个渗滤液的独立年龄和微量元素组成。我们在单个锆石颗粒的一致残留物中观察到~ 50 Myr的年龄不均匀性,以及冥古宙后Pb损失的漫长历史,至少有两个模式大约在~ 0和2-4 Ga。同时,逐级渗滤液微量元素化学分析显示,相对于锆石渣,早期浸出区富集了轻稀土元素、铀、钍和放射性成因铅。除了证实LREE-I蚀变指数的有效性和对化学磨损机制的新认识之外,这些结果的解释和协调表明,Pb的损失主要是由低温水重结晶驱动的,区域热事件可能起着停止而不是开始的作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Geochronology
Geochronology Earth and Planetary Sciences-Paleontology
CiteScore
6.60
自引率
0.00%
发文量
35
审稿时长
19 weeks
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