Tectonophysical and palinspatic sections of the Ukrainian Carpathians along the geo-traverse DOBRE-3 (PANCAKE)

Results of tectonophysical studies and palinspatic reconstruction of the Alpine orogene of the Ukrainian part of the East Carpathians carried out along the international profile DSS PANCAKE which intersects southwestern part of East European craton, East Carpathians and the Pannonian basin are under...

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Datum:2014
Hauptverfasser: Gintov, O.B., Bubnyak, I. N., Vikhot', Yu. M., Murovskaya, A. V., Nakapelyukh, M. V., Shlapinskiy, V. E.
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Sprache:Russisch
Veröffentlicht: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2014
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Online Zugang:https://journals.uran.ua/geofizicheskiy/article/view/116050
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Geofizicheskiy Zhurnal
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author Gintov, O.B.
Bubnyak, I. N.
Vikhot', Yu. M.
Murovskaya, A. V.
Nakapelyukh, M. V.
Shlapinskiy, V. E.
author_facet Gintov, O.B.
Bubnyak, I. N.
Vikhot', Yu. M.
Murovskaya, A. V.
Nakapelyukh, M. V.
Shlapinskiy, V. E.
author_sort Gintov, O.B.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T11:57:19Z
description Results of tectonophysical studies and palinspatic reconstruction of the Alpine orogene of the Ukrainian part of the East Carpathians carried out along the international profile DSS PANCAKE which intersects southwestern part of East European craton, East Carpathians and the Pannonian basin are under consideration. It has been shown that compression forces of southwest and northwest direction which brought to formation of the Ukrainian Carpathians and detected by corresponding regional paleo-tensions began their activity not later than in late Cretaceous. They were accompanied by right and left shifts of the same direction produced by different velocities of northeastward movement of covers parts and skibs. Reconstruction of balanced section of the Ukrainian Carpathians revealed that the primary width of sediments accumulation basin was not less than 460 km i. e. shortening was 340 km, the volume of orogen denudation was 48,1 %. The Pennine clippe belt belongs to the Pennine cover produced from the sediments of the single Pennine-Marmarosh basin as a part of the Carpathian basin of sediments accumulation.
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spelling journalsuranua-geofizicheskiy-article-1160502020-10-07T11:57:19Z Tectonophysical and palinspatic sections of the Ukrainian Carpathians along the geo-traverse DOBRE-3 (PANCAKE) Gintov, O.B. Bubnyak, I. N. Vikhot', Yu. M. Murovskaya, A. V. Nakapelyukh, M. V. Shlapinskiy, V. E. tectonophysic paleotensions palinspatic geodynamic orogene Results of tectonophysical studies and palinspatic reconstruction of the Alpine orogene of the Ukrainian part of the East Carpathians carried out along the international profile DSS PANCAKE which intersects southwestern part of East European craton, East Carpathians and the Pannonian basin are under consideration. It has been shown that compression forces of southwest and northwest direction which brought to formation of the Ukrainian Carpathians and detected by corresponding regional paleo-tensions began their activity not later than in late Cretaceous. They were accompanied by right and left shifts of the same direction produced by different velocities of northeastward movement of covers parts and skibs. Reconstruction of balanced section of the Ukrainian Carpathians revealed that the primary width of sediments accumulation basin was not less than 460 km i. e. shortening was 340 km, the volume of orogen denudation was 48,1 %. The Pennine clippe belt belongs to the Pennine cover produced from the sediments of the single Pennine-Marmarosh basin as a part of the Carpathian basin of sediments accumulation. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2014-06-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116050 10.24028/gzh.0203-3100.v36i3.2014.116050 Geofizicheskiy Zhurnal; Vol. 36 No. 3 (2014); 3-33 Геофизический журнал; Том 36 № 3 (2014); 3-33 Геофізичний журнал; Том 36 № 3 (2014); 3-33 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/116050/110153 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle tectonophysic
paleotensions
palinspatic
geodynamic
orogene
Gintov, O.B.
Bubnyak, I. N.
Vikhot', Yu. M.
Murovskaya, A. V.
Nakapelyukh, M. V.
Shlapinskiy, V. E.
Tectonophysical and palinspatic sections of the Ukrainian Carpathians along the geo-traverse DOBRE-3 (PANCAKE)
title Tectonophysical and palinspatic sections of the Ukrainian Carpathians along the geo-traverse DOBRE-3 (PANCAKE)
title_full Tectonophysical and palinspatic sections of the Ukrainian Carpathians along the geo-traverse DOBRE-3 (PANCAKE)
title_fullStr Tectonophysical and palinspatic sections of the Ukrainian Carpathians along the geo-traverse DOBRE-3 (PANCAKE)
title_full_unstemmed Tectonophysical and palinspatic sections of the Ukrainian Carpathians along the geo-traverse DOBRE-3 (PANCAKE)
title_short Tectonophysical and palinspatic sections of the Ukrainian Carpathians along the geo-traverse DOBRE-3 (PANCAKE)
title_sort tectonophysical and palinspatic sections of the ukrainian carpathians along the geo-traverse dobre-3 (pancake)
topic tectonophysic
paleotensions
palinspatic
geodynamic
orogene
topic_facet tectonophysic
paleotensions
palinspatic
geodynamic
orogene
url https://journals.uran.ua/geofizicheskiy/article/view/116050
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