On the nature of the anomalies of the velocity of propagation of longitudinal seismic waves in the upper mantle

P-velocity models of the upper mantle for the regions with different endogenous regimes on the continents and oceans (Precambrian platforms, zones of young activization, Alpine geosynclines, rifts, deep basins, mid-ocean ridges, margin trenches) have been considered. Thermal models and standard comp...

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Date:2010
Main Author: Gordienko, V. V.
Format: Article
Language:Russian
Published: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2010
Online Access:https://journals.uran.ua/geofizicheskiy/article/view/117556
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Journal Title:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal
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author Gordienko, V. V.
author_facet Gordienko, V. V.
author_sort Gordienko, V. V.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T10:43:09Z
description P-velocity models of the upper mantle for the regions with different endogenous regimes on the continents and oceans (Precambrian platforms, zones of young activization, Alpine geosynclines, rifts, deep basins, mid-ocean ridges, margin trenches) have been considered. Thermal models and standard composition of mantle rocks have been used corresponding to the advection-polymorphous hypothesis. Calculated models are compared with experimental ones, their concordance is demonstrated. The exceptions are the positive anomalies in the experimental data at the depths down to 150-200 km. Perhaps they are connected with the appearance of eclogites in the upper part of the mantle.
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spelling journalsuranua-geofizicheskiy-article-1175562020-10-07T10:43:09Z On the nature of the anomalies of the velocity of propagation of longitudinal seismic waves in the upper mantle Gordienko, V. V. P-velocity models of the upper mantle for the regions with different endogenous regimes on the continents and oceans (Precambrian platforms, zones of young activization, Alpine geosynclines, rifts, deep basins, mid-ocean ridges, margin trenches) have been considered. Thermal models and standard composition of mantle rocks have been used corresponding to the advection-polymorphous hypothesis. Calculated models are compared with experimental ones, their concordance is demonstrated. The exceptions are the positive anomalies in the experimental data at the depths down to 150-200 km. Perhaps they are connected with the appearance of eclogites in the upper part of the mantle. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2010-04-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/117556 10.24028/gzh.0203-3100.v32i2.2010.117556 Geofizicheskiy Zhurnal; Vol. 32 No. 2 (2010); 43-63 Геофизический журнал; Том 32 № 2 (2010); 43-63 Геофізичний журнал; Том 32 № 2 (2010); 43-63 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/117556/111598 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle Gordienko, V. V.
On the nature of the anomalies of the velocity of propagation of longitudinal seismic waves in the upper mantle
title On the nature of the anomalies of the velocity of propagation of longitudinal seismic waves in the upper mantle
title_full On the nature of the anomalies of the velocity of propagation of longitudinal seismic waves in the upper mantle
title_fullStr On the nature of the anomalies of the velocity of propagation of longitudinal seismic waves in the upper mantle
title_full_unstemmed On the nature of the anomalies of the velocity of propagation of longitudinal seismic waves in the upper mantle
title_short On the nature of the anomalies of the velocity of propagation of longitudinal seismic waves in the upper mantle
title_sort on the nature of the anomalies of the velocity of propagation of longitudinal seismic waves in the upper mantle
url https://journals.uran.ua/geofizicheskiy/article/view/117556
work_keys_str_mv AT gordienkovv onthenatureoftheanomaliesofthevelocityofpropagationoflongitudinalseismicwavesintheuppermantle