Uranium-lead dating of granites of the Voznesenskyi massif (the Ingul megablock of the Ukrainian Shield)

Authors

  • L. M. Stepanyuk M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of Ukraine, Kiev
  • V. O. Syomka M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of Ukraine, Kiev
  • S. I. Kurylo M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of Ukraine, Kiev
  • N. A. Donskoy M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of Ukraine, Kiev
  • S. M. Bondarenko M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of Ukraine, Kiev
  • T. I. Dovbush M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of Ukraine, Kiev

DOI:

https://doi.org/10.15407/dopovidi2016.08.079

Keywords:

granite, Ingul megablock, Lysohirskyi massif, monazite, rubidium-strontium isotope system, Ukrainian Shield, uranium-lead dating, Voznesenskyi massif

Abstract

By means of the uranium-lead isotope technique, the dating of monazites from granites of the Voznesenskyi massif is carried out. The age of monazite and, thus, granites is 2034.6 ± 6.6 Ma. The granites were formed of a material of the upper crust according to the primary isotope ratio 87Sr/86Sr2030 (0.71351) for plagioclase from granite.

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References

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Published

15.11.2024

How to Cite

Stepanyuk, L. M., Syomka, V. O., Kurylo, S. I., Donskoy, N. A., Bondarenko, S. M., & Dovbush, T. I. (2024). Uranium-lead dating of granites of the Voznesenskyi massif (the Ingul megablock of the Ukrainian Shield) . Reports of the National Academy of Sciences of Ukraine, (8), 79–84. https://doi.org/10.15407/dopovidi2016.08.079