Deep processes and magmatic activity of the Volyn-Podolian plate
Conditions of formation of basalts of the Volyn-Podolian plate (VPP) have been considered. In Vendian primary melts which were close by their composition to picritic gabbro were differentiated at the depth of 30-35 km during first two stages of activization. The third stage when tuffs of the percali...
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| Дата: | 2010 |
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| Формат: | Стаття |
| Мова: | rus |
| Опубліковано: |
Subbotin Institute of Geophysics of the NAS of Ukraine
2010
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| Онлайн доступ: | https://journals.uran.ua/geofizicheskiy/article/view/117535 |
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| Назва журналу: | Geofizicheskiy Zhurnal |
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Geofizicheskiy Zhurnal| id |
journalsuranua-geofizicheskiy-article-117535 |
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journalsuranua-geofizicheskiy-article-1175352020-10-07T10:58:20Z Deep processes and magmatic activity of the Volyn-Podolian plate Usenko, O. V. Conditions of formation of basalts of the Volyn-Podolian plate (VPP) have been considered. In Vendian primary melts which were close by their composition to picritic gabbro were differentiated at the depth of 30-35 km during first two stages of activization. The third stage when tuffs of the percalian terrain could be produced is not unambiguously subdivided. If the suggested scheme of the process is realized the result of activization in Vendian will be the cold mantle and basic mantle because the melts produced by the upper (crust) asthenosphere are basalts. For explanation of anomalies of paleotemperatures, special features of composition of hydrothermal solutions it is necessary to assume the existence of one more stage (separate activisation) in the territory of VPP. Subbotin Institute of Geophysics of the NAS of Ukraine 2010-06-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/117535 10.24028/gzh.0203-3100.v32i3.2010.117535 Geofizicheskiy Zhurnal; Vol. 32 No. 3 (2010); 66-77 Геофизический журнал; Том 32 № 3 (2010); 66-77 Геофізичний журнал; Том 32 № 3 (2010); 66-77 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/117535/111585 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| institution |
Geofizicheskiy Zhurnal |
| collection |
OJS |
| language |
rus |
| format |
Article |
| author |
Usenko, O. V. |
| spellingShingle |
Usenko, O. V. Deep processes and magmatic activity of the Volyn-Podolian plate |
| author_facet |
Usenko, O. V. |
| author_sort |
Usenko, O. V. |
| title |
Deep processes and magmatic activity of the Volyn-Podolian plate |
| title_short |
Deep processes and magmatic activity of the Volyn-Podolian plate |
| title_full |
Deep processes and magmatic activity of the Volyn-Podolian plate |
| title_fullStr |
Deep processes and magmatic activity of the Volyn-Podolian plate |
| title_full_unstemmed |
Deep processes and magmatic activity of the Volyn-Podolian plate |
| title_sort |
deep processes and magmatic activity of the volyn-podolian plate |
| description |
Conditions of formation of basalts of the Volyn-Podolian plate (VPP) have been considered. In Vendian primary melts which were close by their composition to picritic gabbro were differentiated at the depth of 30-35 km during first two stages of activization. The third stage when tuffs of the percalian terrain could be produced is not unambiguously subdivided. If the suggested scheme of the process is realized the result of activization in Vendian will be the cold mantle and basic mantle because the melts produced by the upper (crust) asthenosphere are basalts. For explanation of anomalies of paleotemperatures, special features of composition of hydrothermal solutions it is necessary to assume the existence of one more stage (separate activisation) in the territory of VPP. |
| publisher |
Subbotin Institute of Geophysics of the NAS of Ukraine |
| publishDate |
2010 |
| url |
https://journals.uran.ua/geofizicheskiy/article/view/117535 |
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2024-04-21T19:41:52Z |
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2024-04-21T19:41:52Z |
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