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
Автори: Bakhmutov, V. G., Teiser-Elenskaya, M., Kadzyalko-Hofmokl, M., Konstantinenko, L., Polyachenko, E. B.
Формат: Стаття
Мова:rus
Опубліковано: Subbotin Institute of Geophysics of the NAS of Ukraine 2012
Онлайн доступ:https://journals.uran.ua/geofizicheskiy/article/view/116703
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Назва журналу:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal
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spelling 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
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first_indexed 2024-04-21T19:41:13Z
last_indexed 2024-04-21T19:41:13Z
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