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STRATI 2013 pp 903-907 | Cite as

On the Problems of Correlating the Pleistocene Glacial Deposits in the Russian Altai with Siberian Stratigraphic Scales

  • A. R. AgatovaEmail author
  • R. K. Nepop
  • H. Rodnight
Conference paper
Part of the Springer Geology book series (SPRINGERGEOL)

Abstract

Thermoluminescence (TL), infrared stimulated luminescence (IRSL), and 14C dates obtained for the Pleistocene glacial deposits from the Chagan section (Russian Altai) and previously published dates demonstrate the considerable complexity of the absolute dating of such sediments. These results cast doubt on available depositional correlation schemes for the Russian Altai and Siberia based on TL dating.

Keywords

Pleistocene Glacial sedimentation TL IRSL Radiocarbon dating Russian Altai 

Notes

Acknowledgments

The study was funded by RFBR foundation (grant 13-05-00555).

References

  1. Agatova, A. R. (2005). Geomorphologic mapping of the Chagan-Uzun river basin: a key for reconstructing history of Pleistocene glaciations in the Southeastern Altai. Stratigraphy and Geological Correlation,13(6), 656–666.Google Scholar
  2. Agatova, A. R., Devyatkin, E. V., Vysotsky, E. M., Skobelitcin, G. A., & Nepop, R. K. (2004). Results of using TL method for dating glacial sediments of the Chagan section (SE Altai). Proceedings 38 Plenum of Geomorphological commission,Novosibirsk (pp. 7–9). (In Russian).Google Scholar
  3. Agatova, A. R., Nepop, R. K., & Vysotsky, E. M. (2006). Seismogravitational paleodislocations in Chagan River valley. Russian geomorphology,4, 53–62. (In Russian).Google Scholar
  4. Devyatkin, E. V. (1965). Cenozoic deposits and neotectonics of Southeastern Altai (p. 244). Moscow: USSR Academy of Science Publisher. (In Russian).Google Scholar
  5. Rusanov, G. G. (2008). The highest level of the Chuya glacial dammed lake in Gorny Altai. Russian Geomorphology,1, 65–71. (In Russian).Google Scholar
  6. Sheinkman, V. S. (2002). Testing of the S–S technology of TL dating on Dead Sea shore’s sections, its using in Gorny Altai and paleogeographical interpretation of the results. Archeology, Etnography and Anthropology of Eurasia,2(10), 22–37. (In Russian).Google Scholar
  7. Svitoch, A. A., Boyarskaya, T. D., Voskresenskaya, T. N., Glushankova, I. I., Evseev AV, & Kursalova, V. I. et al. (1978). The sections of the latest deposits of Altai (p. 208). Moscow: MSU Publisher. (In Russian).Google Scholar
  8. Thomsen, K. J., Murray, A. S., Jain, M., & Bøtter-Jensen, L. (2008). Laboratory fading rates of various luminescence signals from feldspar-rich sediment extracts. Radiation Measurements,43, 1474–1486.CrossRefGoogle Scholar

Copyright information

© Springer-Verlag Berlin Heidelberg 2014

Authors and Affiliations

  1. 1.Institute of Geology and MineralogyNovosibirskRussia
  2. 2.Institute for Geology and PalaeontologyUniversity of InnsbruckInnsbruckAustria

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