芬兰南部变质岩的新年龄制约因素

IF 1.3 4区 地球科学 Q2 GEOLOGY
Paula Salminen, M. Kurhila
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引用次数: 0

摘要

对芬兰南部九个采样点的沉积岩和其中一个采样点的中间堤坝进行了采样,以分析 U-Pb 锆石年龄和地球化学成分。沉积岩样本的锆石得出的 207Pb/206Pb 时间范围为 3281 至 1810 Ma。来自表观碎屑锆石岩心的近乎一致的年代表明了一个年龄约为 2.1-2.0 Ga 的突出来源。六个变质岩样本的最大沉积年龄估计在 1.96 至 1.89 Ga 之间。变质岩样本中的锆石边缘和覆盖层以及变质锆石的数据表明,研究区域至少在约 1.89 和 1.84 Ga 发生过区域变质事件。1.89和1.84 Ga,也可能是在约1.87 Ga。1.87 Ga。沉积的最小年龄(≤1.89 Ga)是根据区域变质作用和侵入岩的年龄估算出来的。一些锆石边缘和覆盖层的 207Pb/206Pb 时间≥1.91 Ga,被认为可能代表了源区的变质事件。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
New age constraints for metasedimentary rocks in southern Finland
Metasedimentary rocks from nine sampling sites in southern Finland and an intermediate dyke in one of these sites were sampled for analysis of U–Pb zircon age and geochemical composition. The zircons of the metasedimentary rock samples yield 207Pb/206Pb dates ranging from 3281 to 1810 Ma. The nearly concordant dates from apparent detrital zircon cores indicate a prominent source with age around 2.1–2.0 Ga. The maximum depositional ages estimated for six of the metasedimentary rock samples span from 1.96 to 1.89 Ga. The data from zircon rims and overgrowths and metamorphic zircons in the metasedimentary rock samples indicate regional metamorphic events in the study area at least at ca. 1.89 and 1.84 Ga, and possibly also at ca. 1.87 Ga. The minimum age of the deposition (≤1.89 Ga) was estimated based on the ages of the regional metamorphism and the intrusive rocks. Some zircon rims and overgrowths yield ≥1.91 Ga 207Pb/206Pb dates, which are considered to possibly represent metamorphic events in the source areas.
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来源期刊
CiteScore
1.30
自引率
0.00%
发文量
5
审稿时长
>12 weeks
期刊介绍: Bulletin of the Geological Society of Finland (BGSF) publishes research articles and short communications in all branches of geosciences. Contributions from outside Finland are welcome, provided that they contain material relevant to Finnish geology or are of general interest.
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