Some mineralogical data on genesis of magmas of the Carpathian region
A brief characteristics of minerals of magmatic rocks is given: pyroxenes, olivine, spinel, garnet, tridymite. Composition of clinopyroxenes indicates two geodynamic regimes in Mesozoic: intraplate (continental crust destruction) and spreading one (partial break of oceanic crust). Garnet from Miocen...
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| Datum: | 2010 |
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| Format: | Artikel |
| Sprache: | Russisch |
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S. Subbotin Institute of Geophysics of the NAS of Ukraine
2010
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| Online Zugang: | https://journals.uran.ua/geofizicheskiy/article/view/117546 |
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| Назва журналу: | Geofizicheskiy Zhurnal |
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Geofizicheskiy Zhurnal| _version_ | 1856543348876115968 |
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| author | Lyashkevich, Z. M. |
| author_facet | Lyashkevich, Z. M. |
| author_sort | Lyashkevich, Z. M. |
| baseUrl_str | |
| collection | OJS |
| datestamp_date | 2020-10-07T10:58:20Z |
| description | A brief characteristics of minerals of magmatic rocks is given: pyroxenes, olivine, spinel, garnet, tridymite. Composition of clinopyroxenes indicates two geodynamic regimes in Mesozoic: intraplate (continental crust destruction) and spreading one (partial break of oceanic crust). Garnet from Miocene rhyodacites crystallized within the apical part of magmatic source at high pressure. Presence of tridymite testifies to high, about 1400°С temperatures of acid melts eruption. |
| first_indexed | 2025-07-17T11:09:08Z |
| format | Article |
| id | journalsuranua-geofizicheskiy-article-117546 |
| institution | Geofizicheskiy Zhurnal |
| language | Russian |
| last_indexed | 2025-07-17T11:09:08Z |
| publishDate | 2010 |
| publisher | S. Subbotin Institute of Geophysics of the NAS of Ukraine |
| record_format | ojs |
| spelling | journalsuranua-geofizicheskiy-article-1175462020-10-07T10:58:20Z Some mineralogical data on genesis of magmas of the Carpathian region Lyashkevich, Z. M. A brief characteristics of minerals of magmatic rocks is given: pyroxenes, olivine, spinel, garnet, tridymite. Composition of clinopyroxenes indicates two geodynamic regimes in Mesozoic: intraplate (continental crust destruction) and spreading one (partial break of oceanic crust). Garnet from Miocene rhyodacites crystallized within the apical part of magmatic source at high pressure. Presence of tridymite testifies to high, about 1400°С temperatures of acid melts eruption. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2010-06-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/117546 10.24028/gzh.0203-3100.v32i3.2010.117546 Geofizicheskiy Zhurnal; Vol. 32 No. 3 (2010); 136-139 Геофизический журнал; Том 32 № 3 (2010); 136-139 Геофізичний журнал; Том 32 № 3 (2010); 136-139 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/117546/111593 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| spellingShingle | Lyashkevich, Z. M. Some mineralogical data on genesis of magmas of the Carpathian region |
| title | Some mineralogical data on genesis of magmas of the Carpathian region |
| title_full | Some mineralogical data on genesis of magmas of the Carpathian region |
| title_fullStr | Some mineralogical data on genesis of magmas of the Carpathian region |
| title_full_unstemmed | Some mineralogical data on genesis of magmas of the Carpathian region |
| title_short | Some mineralogical data on genesis of magmas of the Carpathian region |
| title_sort | some mineralogical data on genesis of magmas of the carpathian region |
| url | https://journals.uran.ua/geofizicheskiy/article/view/117546 |
| work_keys_str_mv | AT lyashkevichzm somemineralogicaldataongenesisofmagmasofthecarpathianregion |