Intermediate earthquakes of the Vrancea zone and high-speed structure of the mantle of Eastern Europe

New data on the possible relationship of intermediate earthquakes of the Vrancea zone with the velocity structure of the mantle based on a three-dimensional P-velocity model of the mantle up to a depth of 850 km, have been given in the paper not only for the immediate environment (Vrancea area has b...

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Datum:2013
Hauptverfasser: Starostenko, V. I., Kendzera, A. V., Tsvetkova, T.A., Bugaenko, I. V.
Format: Artikel
Sprache:Russisch
Veröffentlicht: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2013
Online Zugang:https://journals.uran.ua/geofizicheskiy/article/view/116392
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author Starostenko, V. I.
Kendzera, A. V.
Tsvetkova, T.A.
Bugaenko, I. V.
author_facet Starostenko, V. I.
Kendzera, A. V.
Tsvetkova, T.A.
Bugaenko, I. V.
author_sort Starostenko, V. I.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T12:00:36Z
description New data on the possible relationship of intermediate earthquakes of the Vrancea zone with the velocity structure of the mantle based on a three-dimensional P-velocity model of the mantle up to a depth of 850 km, have been given in the paper not only for the immediate environment (Vrancea area has been shown as the contact boundary region), but also for the wider region (the relationship of the Vrancea zone with the velocity structure of the mantle of the Afro-Ara-bian, East European platforms, the Adriatic microplate and the Scythian-Turan plate have been shown).
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spelling journalsuranua-geofizicheskiy-article-1163922020-10-07T12:00:36Z Intermediate earthquakes of the Vrancea zone and high-speed structure of the mantle of Eastern Europe Starostenko, V. I. Kendzera, A. V. Tsvetkova, T.A. Bugaenko, I. V. New data on the possible relationship of intermediate earthquakes of the Vrancea zone with the velocity structure of the mantle based on a three-dimensional P-velocity model of the mantle up to a depth of 850 km, have been given in the paper not only for the immediate environment (Vrancea area has been shown as the contact boundary region), but also for the wider region (the relationship of the Vrancea zone with the velocity structure of the mantle of the Afro-Ara-bian, East European platforms, the Adriatic microplate and the Scythian-Turan plate have been shown). S. Subbotin Institute of Geophysics of the NAS of Ukraine 2013-04-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116392 10.24028/gzh.0203-3100.v35i3.2013.116392 Geofizicheskiy Zhurnal; Vol. 35 No. 3 (2013); 31-45 Геофизический журнал; Том 35 № 3 (2013); 31-45 Геофізичний журнал; Том 35 № 3 (2013); 31-45 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/116392/110443 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle Starostenko, V. I.
Kendzera, A. V.
Tsvetkova, T.A.
Bugaenko, I. V.
Intermediate earthquakes of the Vrancea zone and high-speed structure of the mantle of Eastern Europe
title Intermediate earthquakes of the Vrancea zone and high-speed structure of the mantle of Eastern Europe
title_full Intermediate earthquakes of the Vrancea zone and high-speed structure of the mantle of Eastern Europe
title_fullStr Intermediate earthquakes of the Vrancea zone and high-speed structure of the mantle of Eastern Europe
title_full_unstemmed Intermediate earthquakes of the Vrancea zone and high-speed structure of the mantle of Eastern Europe
title_short Intermediate earthquakes of the Vrancea zone and high-speed structure of the mantle of Eastern Europe
title_sort intermediate earthquakes of the vrancea zone and high-speed structure of the mantle of eastern europe
url https://journals.uran.ua/geofizicheskiy/article/view/116392
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AT tsvetkovata intermediateearthquakesofthevranceazoneandhighspeedstructureofthemantleofeasterneurope
AT bugaenkoiv intermediateearthquakesofthevranceazoneandhighspeedstructureofthemantleofeasterneurope