The structure of velocity mantle number of horizons under Phennoscandia according to seismic-tomography data
Seismic boundaries of the second kind have been distinguished under Phennoscandia according to three-dimensional P-velocity model of the mantle and velocity number of horizons of the upper mantle and its transitional zone has been shown. Four velocity horizons and corresponding seismic boundaries of...
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| Дата: | 2016 |
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| Автори: | , |
| Формат: | Стаття |
| Мова: | rus |
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Subbotin Institute of Geophysics of the NAS of Ukraine
2016
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| Онлайн доступ: | https://journals.uran.ua/geofizicheskiy/article/view/107723 |
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| Назва журналу: | Geofizicheskiy Zhurnal |
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Geofizicheskiy Zhurnal| id |
journalsuranua-geofizicheskiy-article-107723 |
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ojs |
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journalsuranua-geofizicheskiy-article-1077232020-10-07T11:35:07Z The structure of velocity mantle number of horizons under Phennoscandia according to seismic-tomography data Tsvetkova, T. A. Bugaenko, I. V. seismic tomography seismic boundaries of the second kind Seismic boundaries of the second kind have been distinguished under Phennoscandia according to three-dimensional P-velocity model of the mantle and velocity number of horizons of the upper mantle and its transitional zone has been shown. Four velocity horizons and corresponding seismic boundaries of the second kind have been distinguished. It has been shown that within the limits of the upper mantle the market boundaries correspond to the known ones, distinguished by the super-long profiles: Phennolora, Quartz, Ruby and Svekalapka massif. Seismic boundaries of the second kind of transitional zone have been marked. Subbotin Institute of Geophysics of the NAS of Ukraine 2016-02-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/107723 10.24028/gzh.0203-3100.v38i1.2016.107723 Geofizicheskiy Zhurnal; Vol. 38 No. 1 (2016); 57-77 Геофизический журнал; Том 38 № 1 (2016); 57-77 Геофізичний журнал; Том 38 № 1 (2016); 57-77 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/107723/102691 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| institution |
Geofizicheskiy Zhurnal |
| collection |
OJS |
| language |
rus |
| topic |
seismic tomography seismic boundaries of the second kind |
| spellingShingle |
seismic tomography seismic boundaries of the second kind Tsvetkova, T. A. Bugaenko, I. V. The structure of velocity mantle number of horizons under Phennoscandia according to seismic-tomography data |
| topic_facet |
seismic tomography seismic boundaries of the second kind |
| format |
Article |
| author |
Tsvetkova, T. A. Bugaenko, I. V. |
| author_facet |
Tsvetkova, T. A. Bugaenko, I. V. |
| author_sort |
Tsvetkova, T. A. |
| title |
The structure of velocity mantle number of horizons under Phennoscandia according to seismic-tomography data |
| title_short |
The structure of velocity mantle number of horizons under Phennoscandia according to seismic-tomography data |
| title_full |
The structure of velocity mantle number of horizons under Phennoscandia according to seismic-tomography data |
| title_fullStr |
The structure of velocity mantle number of horizons under Phennoscandia according to seismic-tomography data |
| title_full_unstemmed |
The structure of velocity mantle number of horizons under Phennoscandia according to seismic-tomography data |
| title_sort |
structure of velocity mantle number of horizons under phennoscandia according to seismic-tomography data |
| description |
Seismic boundaries of the second kind have been distinguished under Phennoscandia according to three-dimensional P-velocity model of the mantle and velocity number of horizons of the upper mantle and its transitional zone has been shown. Four velocity horizons and corresponding seismic boundaries of the second kind have been distinguished. It has been shown that within the limits of the upper mantle the market boundaries correspond to the known ones, distinguished by the super-long profiles: Phennolora, Quartz, Ruby and Svekalapka massif. Seismic boundaries of the second kind of transitional zone have been marked. |
| publisher |
Subbotin Institute of Geophysics of the NAS of Ukraine |
| publishDate |
2016 |
| url |
https://journals.uran.ua/geofizicheskiy/article/view/107723 |
| work_keys_str_mv |
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2024-04-21T19:39:35Z |
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2024-04-21T19:39:35Z |
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