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The earthquake in L'Aquila and the features of the three-dimensional P-velocity structure of the mantle beneath the Adriatic plate and its environment

The earthquake in L'Aquila and the features of the three-dimensional P-velocity structure of the mantle beneath the Adriatic plate and its environment

Confinement of the surface (crustal) earthquake happened on April 25 2009 in the area of the city Aquila in Italy to deep mantle processes under this area has been shown, which have been analyzed on the basis of three-dimensional P-velocity model of the mantle up to the depth of 2,500 km. This earth...

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Main Authors: Starostenko, V. I., Kendzera, A. V., Bugaenko, I. V., Tsvetkova, T. A.
Format: Article
Language:rus
Published: Subbotin Institute of Geophysics of the NAS of Ukraine 2011
Online Access:https://journals.uran.ua/geofizicheskiy/article/view/116896
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spelling journalsuranua-geofizicheskiy-article-1168962020-10-07T11:02:11Z The earthquake in L'Aquila and the features of the three-dimensional P-velocity structure of the mantle beneath the Adriatic plate and its environment Starostenko, V. I. Kendzera, A. V. Bugaenko, I. V. Tsvetkova, T. A. Confinement of the surface (crustal) earthquake happened on April 25 2009 in the area of the city Aquila in Italy to deep mantle processes under this area has been shown, which have been analyzed on the basis of three-dimensional P-velocity model of the mantle up to the depth of 2,500 km. This earthquake is confined to the area, which is characterized by certain sub-vertical dividing zone in the mantle where alternation (along the lateral) of the areas with high and low velocities takes place throughout all the depths Subbotin Institute of Geophysics of the NAS of Ukraine 2011-08-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116896 10.24028/gzh.0203-3100.v33i4.2011.116896 Geofizicheskiy Zhurnal; Vol. 33 No. 4 (2011); 62-73 Геофизический журнал; Том 33 № 4 (2011); 62-73 Геофізичний журнал; Том 33 № 4 (2011); 62-73 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/116896/110942 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
institution Geofizicheskiy Zhurnal
collection OJS
language rus
format Article
author Starostenko, V. I.
Kendzera, A. V.
Bugaenko, I. V.
Tsvetkova, T. A.
spellingShingle Starostenko, V. I.
Kendzera, A. V.
Bugaenko, I. V.
Tsvetkova, T. A.
The earthquake in L'Aquila and the features of the three-dimensional P-velocity structure of the mantle beneath the Adriatic plate and its environment
author_facet Starostenko, V. I.
Kendzera, A. V.
Bugaenko, I. V.
Tsvetkova, T. A.
author_sort Starostenko, V. I.
title The earthquake in L'Aquila and the features of the three-dimensional P-velocity structure of the mantle beneath the Adriatic plate and its environment
title_short The earthquake in L'Aquila and the features of the three-dimensional P-velocity structure of the mantle beneath the Adriatic plate and its environment
title_full The earthquake in L'Aquila and the features of the three-dimensional P-velocity structure of the mantle beneath the Adriatic plate and its environment
title_fullStr The earthquake in L'Aquila and the features of the three-dimensional P-velocity structure of the mantle beneath the Adriatic plate and its environment
title_full_unstemmed The earthquake in L'Aquila and the features of the three-dimensional P-velocity structure of the mantle beneath the Adriatic plate and its environment
title_sort earthquake in l'aquila and the features of the three-dimensional p-velocity structure of the mantle beneath the adriatic plate and its environment
description Confinement of the surface (crustal) earthquake happened on April 25 2009 in the area of the city Aquila in Italy to deep mantle processes under this area has been shown, which have been analyzed on the basis of three-dimensional P-velocity model of the mantle up to the depth of 2,500 km. This earthquake is confined to the area, which is characterized by certain sub-vertical dividing zone in the mantle where alternation (along the lateral) of the areas with high and low velocities takes place throughout all the depths
publisher Subbotin Institute of Geophysics of the NAS of Ukraine
publishDate 2011
url https://journals.uran.ua/geofizicheskiy/article/view/116896
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first_indexed 2024-04-21T19:41:30Z
last_indexed 2024-04-21T19:41:30Z
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