Paleomagnetic studies of the Lower Devonian gray deposits of Podolia

Authors

  • V. G. Bakhmutov Institute of Geophysics of the National Academy of Sciences of Ukraine, Ukraine
  • M. Teiser-Elenskaya Institute of Geophysics, Polish Academy of Sciences, Poland
  • M. Kadzyalko-Hofmokl Institute of Geophysics, Polish Academy of Sciences, Poland
  • L. Konstantinenko Institute of Geological Sciences of the National Academy of Sciences of Ukraine, Ukraine
  • E. B. Polyachenko Institute of Geophysics of the National Academy of Sciences of Ukraine, Ukraine

DOI:

https://doi.org/10.24028/gzh.0203-3100.v34i6.2012.116703

Abstract

New results of paleomagnetic studies of Lower Devonian sediments from the southwest of Ukraine (the Podolia area, the Dniester river basin) have been presented. The samples are grey limestone and dolomite of Tiverian series comparable with the Lochkovian stage of the Geological time scale. Stable component of magnetization of the most samples indicate to remagnetization of rocks (the Permian pole, ϕ=45qS, λ=340qE, dp/dm=2q/5q). In some samples of the Ivanev suite the primary component of magnetization (Lower Devonian direction) has been distinguished. Paleomag-netic pole (ϕ=0q, λ=329qE, dp/dm=10q/12q) is in a good agreement with Lower Devonian fragment of apparent wander path for the Baltica. The results are in agreement with earlier data of authors for Silurian gray sedimentary rocks of Podolia.

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Published

2012-12-01

How to Cite

Bakhmutov, V. G., Teiser-Elenskaya, M., Kadzyalko-Hofmokl, M., Konstantinenko, L., & Polyachenko, E. B. (2012). Paleomagnetic studies of the Lower Devonian gray deposits of Podolia. Geofizicheskiy Zhurnal, 34(6), 57–67. https://doi.org/10.24028/gzh.0203-3100.v34i6.2012.116703

Issue

Vol. 34 No. 6 (2012)

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