Paleomagnetic studies of the Lower Devonian gray deposits of Podolia
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 co...
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Дата: | 2012 |
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Subbotin Institute of Geophysics of the NAS of Ukraine
2012
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journalsuranua-geofizicheskiy-article-1167032020-10-07T12:21:02Z Paleomagnetic studies of the Lower Devonian gray deposits of Podolia Bakhmutov, V. G. Teiser-Elenskaya, M. Kadzyalko-Hofmokl, M. Konstantinenko, L. Polyachenko, E. B. 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. Subbotin Institute of Geophysics of the NAS of Ukraine 2012-12-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116703 10.24028/gzh.0203-3100.v34i6.2012.116703 Geofizicheskiy Zhurnal; Vol. 34 No. 6 (2012); 57-67 Геофизический журнал; Том 34 № 6 (2012); 57-67 Геофізичний журнал; Том 34 № 6 (2012); 57-67 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/116703/110760 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
institution |
Geofizicheskiy Zhurnal |
collection |
OJS |
language |
rus |
format |
Article |
author |
Bakhmutov, V. G. Teiser-Elenskaya, M. Kadzyalko-Hofmokl, M. Konstantinenko, L. Polyachenko, E. B. |
spellingShingle |
Bakhmutov, V. G. Teiser-Elenskaya, M. Kadzyalko-Hofmokl, M. Konstantinenko, L. Polyachenko, E. B. Paleomagnetic studies of the Lower Devonian gray deposits of Podolia |
author_facet |
Bakhmutov, V. G. Teiser-Elenskaya, M. Kadzyalko-Hofmokl, M. Konstantinenko, L. Polyachenko, E. B. |
author_sort |
Bakhmutov, V. G. |
title |
Paleomagnetic studies of the Lower Devonian gray deposits of Podolia |
title_short |
Paleomagnetic studies of the Lower Devonian gray deposits of Podolia |
title_full |
Paleomagnetic studies of the Lower Devonian gray deposits of Podolia |
title_fullStr |
Paleomagnetic studies of the Lower Devonian gray deposits of Podolia |
title_full_unstemmed |
Paleomagnetic studies of the Lower Devonian gray deposits of Podolia |
title_sort |
paleomagnetic studies of the lower devonian gray deposits of podolia |
description |
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. |
publisher |
Subbotin Institute of Geophysics of the NAS of Ukraine |
publishDate |
2012 |
url |
https://journals.uran.ua/geofizicheskiy/article/view/116703 |
work_keys_str_mv |
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first_indexed |
2024-04-21T19:41:13Z |
last_indexed |
2024-04-21T19:41:13Z |
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