Velocity sections of the upper mantle under the oceans

We constructed the models of the distribution of longitudinal seismic waves velocities for the upper mantle oceanic regions: mid-ocean ridges (MOR), basins, trenches, island arcs and coastal ridges, back-arc troughs (BAT). They are in line with the schemes of advection-polymorphic deepseated process...

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Бібліографічні деталі
Дата:2016
Автори: Gordienko, V.V., Gordienko, L.Ya.
Формат: Стаття
Мова:rus
Опубліковано: Subbotin Institute of Geophysics of the NAS of Ukraine 2016
Теми:
Онлайн доступ:https://journals.uran.ua/geofizicheskiy/article/view/91964
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Назва журналу:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal
id journalsuranua-geofizicheskiy-article-91964
record_format ojs
spelling journalsuranua-geofizicheskiy-article-919642020-10-07T11:18:21Z Velocity sections of the upper mantle under the oceans Gordienko, V.V. Gordienko, L.Ya. oceans upper mantle velocity models deep-seated processes We constructed the models of the distribution of longitudinal seismic waves velocities for the upper mantle oceanic regions: mid-ocean ridges (MOR), basins, trenches, island arcs and coastal ridges, back-arc troughs (BAT). They are in line with the schemes of advection-polymorphic deepseated processes in tectonosphere. Under the island arcs and coastal ridges models meet the alpine geosyncline supplemented with recent activization. Under the MOR and BAT the models coincide. They correspond to the scheme of recent heat and mass transfer for rifting which on the mafic crust with continental thickness leads to oceanization. The basin model shows the result of smoothing of thermal anomalies under the MOR or BAT in about 50 100 million years. The trench model corresponds to the result of lateral warming-up of upper layers of the mantle of the inactive blocks from the island arc and basin Subbotin Institute of Geophysics of the NAS of Ukraine 2016-12-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/91964 10.24028/gzh.0203-3100.v38i6.2016.91964 Geofizicheskiy Zhurnal; Vol. 38 No. 6 (2016); 64-82 Геофизический журнал; Том 38 № 6 (2016); 64-82 Геофізичний журнал; Том 38 № 6 (2016); 64-82 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/91964/87742 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
institution Geofizicheskiy Zhurnal
collection OJS
language rus
topic oceans
upper mantle
velocity models
deep-seated processes
spellingShingle oceans
upper mantle
velocity models
deep-seated processes
Gordienko, V.V.
Gordienko, L.Ya.
Velocity sections of the upper mantle under the oceans
topic_facet oceans
upper mantle
velocity models
deep-seated processes
format Article
author Gordienko, V.V.
Gordienko, L.Ya.
author_facet Gordienko, V.V.
Gordienko, L.Ya.
author_sort Gordienko, V.V.
title Velocity sections of the upper mantle under the oceans
title_short Velocity sections of the upper mantle under the oceans
title_full Velocity sections of the upper mantle under the oceans
title_fullStr Velocity sections of the upper mantle under the oceans
title_full_unstemmed Velocity sections of the upper mantle under the oceans
title_sort velocity sections of the upper mantle under the oceans
description We constructed the models of the distribution of longitudinal seismic waves velocities for the upper mantle oceanic regions: mid-ocean ridges (MOR), basins, trenches, island arcs and coastal ridges, back-arc troughs (BAT). They are in line with the schemes of advection-polymorphic deepseated processes in tectonosphere. Under the island arcs and coastal ridges models meet the alpine geosyncline supplemented with recent activization. Under the MOR and BAT the models coincide. They correspond to the scheme of recent heat and mass transfer for rifting which on the mafic crust with continental thickness leads to oceanization. The basin model shows the result of smoothing of thermal anomalies under the MOR or BAT in about 50 100 million years. The trench model corresponds to the result of lateral warming-up of upper layers of the mantle of the inactive blocks from the island arc and basin
publisher Subbotin Institute of Geophysics of the NAS of Ukraine
publishDate 2016
url https://journals.uran.ua/geofizicheskiy/article/view/91964
work_keys_str_mv AT gordienkovv velocitysectionsoftheuppermantleundertheoceans
AT gordienkolya velocitysectionsoftheuppermantleundertheoceans
first_indexed 2024-04-21T19:39:46Z
last_indexed 2024-04-21T19:39:46Z
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