Experience of chemical Th-U-Pb chemical dating of zircon from metasomatic felsic veins of the Mridino area, Belomorian eclogite province

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• 作者：V. V. Khiller ; V. V. Reverdatto ; A. N. Konilov ; A. A. Viryus…
• 刊名：Doklady Earth Sciences
• 出版年：2015
• 出版时间：May 2015
• 年：2015
• 卷：462
• 期：1
• 页码：494-496
• 全文大小：279 KB
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• 作者单位：V. V. Khiller (1)
  V. V. Reverdatto (2)
  A. N. Konilov (3) (4)
  A. A. Viryus (4)
  K. A. Dokukina (3)
  K. V. Van (4)
  I. M. Romanenko (4)
  
  1. Zavaritskii Institute of Geology and Geochemistry, Ural Branch, Russian Academy of Sciences, Pochtovyi per. 7, Yekaterinburg, 620075, Russia
  2. Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia
  3. Geological Institute, Russian Academy of Sciences, Pyzhevskii per. 7, Moscow, 119017, Russia
  4. Institute of Experimental Mineralogy, ul. Akademika Osip’yana 4, Chernogolovka, Moscow oblast, 142432, Russia
  
• 刊物主题：Earth Sciences, general;
• 出版者：Springer US
• ISSN：1531-8354

文摘

For the first time in Russia, the Th-U-Pb isochron and point ages of zircons with anomalous U, Th, Pb, Y, and REE contents were determined by chemical dating. Zircons were extracted from metasomatic veinlets, which cut the eclogitized dike of olivine gabbronorites. The Paleoproterozoic ages (?400, 2100, and 1890 Ma) are quite consistent with the previously determined U-Pb SHRIMP II age of these zircons.