Thermal flow and geothermic models of the earth’s crust of the Ukrainian Carpathians
Within the limits of the Ukrainian sector of the East Carpathians and adjacent edge of the East European platform thermal flows vary from 35 to 130 mVt/m2. It has been shown on the base of geological-geophysical analysis and mathematical modeling of the heat flow that the principal regularities in d...
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| Дата: | 2014 |
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| Автор: | |
| Формат: | Стаття |
| Мова: | Російська |
| Опубліковано: |
S. Subbotin Institute of Geophysics of the NAS of Ukraine
2014
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| Онлайн доступ: | https://journals.uran.ua/geofizicheskiy/article/view/111016 |
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| Назва журналу: | Geofizicheskiy Zhurnal |
Репозитарії
Geofizicheskiy Zhurnal| _version_ | 1856543132144893952 |
|---|---|
| author | Kutas, R.I. |
| author_facet | Kutas, R.I. |
| author_sort | Kutas, R.I. |
| baseUrl_str | |
| collection | OJS |
| datestamp_date | 2020-10-07T11:45:12Z |
| description | Within the limits of the Ukrainian sector of the East Carpathians and adjacent edge of the East European platform thermal flows vary from 35 to 130 mVt/m2. It has been shown on the base of geological-geophysical analysis and mathematical modeling of the heat flow that the principal regularities in distribution of thermal flow are controlled by regional tectonic zoning, which was formed by the process of geological development of the region. Low values of heat flow correspond to the structures with earth’s crust produced in Precambrian and Early Paleozoic (the slope of Precambrian platform and considerable parts of Pre-Carpathian flexure and external flysh Carpathians). Variations of thermal flow within the Folded Carpathians are possibly stipulated by lateral changes of heat generation or heat conductivity within sedimentary layer. High thermal flows in the Pannonian basin are associated with special features of tectonic evolution of lithosphere and earth’s crust during the Alpine stage and with magmatic activity. The increase of thermal flow is conditioned by stretching of the earth’s crust and lifting of asthenosphere. |
| first_indexed | 2025-07-17T11:05:04Z |
| format | Article |
| id | journalsuranua-geofizicheskiy-article-111016 |
| institution | Geofizicheskiy Zhurnal |
| language | Russian |
| last_indexed | 2025-07-17T11:05:04Z |
| publishDate | 2014 |
| publisher | S. Subbotin Institute of Geophysics of the NAS of Ukraine |
| record_format | ojs |
| spelling | journalsuranua-geofizicheskiy-article-1110162020-10-07T11:45:12Z Thermal flow and geothermic models of the earth’s crust of the Ukrainian Carpathians Kutas, R.I. Carpathians temperature thermal flow geothermic model the earth’s crust Within the limits of the Ukrainian sector of the East Carpathians and adjacent edge of the East European platform thermal flows vary from 35 to 130 mVt/m2. It has been shown on the base of geological-geophysical analysis and mathematical modeling of the heat flow that the principal regularities in distribution of thermal flow are controlled by regional tectonic zoning, which was formed by the process of geological development of the region. Low values of heat flow correspond to the structures with earth’s crust produced in Precambrian and Early Paleozoic (the slope of Precambrian platform and considerable parts of Pre-Carpathian flexure and external flysh Carpathians). Variations of thermal flow within the Folded Carpathians are possibly stipulated by lateral changes of heat generation or heat conductivity within sedimentary layer. High thermal flows in the Pannonian basin are associated with special features of tectonic evolution of lithosphere and earth’s crust during the Alpine stage and with magmatic activity. The increase of thermal flow is conditioned by stretching of the earth’s crust and lifting of asthenosphere. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2014-12-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/111016 10.24028/gzh.0203-3100.v36i6.2014.111016 Geofizicheskiy Zhurnal; Vol. 36 No. 6 (2014); 3-27 Геофизический журнал; Том 36 № 6 (2014); 3-27 Геофізичний журнал; Том 36 № 6 (2014); 3-27 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/111016/105943 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| spellingShingle | Carpathians temperature thermal flow geothermic model the earth’s crust Kutas, R.I. Thermal flow and geothermic models of the earth’s crust of the Ukrainian Carpathians |
| title | Thermal flow and geothermic models of the earth’s crust of the Ukrainian Carpathians |
| title_full | Thermal flow and geothermic models of the earth’s crust of the Ukrainian Carpathians |
| title_fullStr | Thermal flow and geothermic models of the earth’s crust of the Ukrainian Carpathians |
| title_full_unstemmed | Thermal flow and geothermic models of the earth’s crust of the Ukrainian Carpathians |
| title_short | Thermal flow and geothermic models of the earth’s crust of the Ukrainian Carpathians |
| title_sort | thermal flow and geothermic models of the earth’s crust of the ukrainian carpathians |
| topic | Carpathians temperature thermal flow geothermic model the earth’s crust |
| topic_facet | Carpathians temperature thermal flow geothermic model the earth’s crust |
| url | https://journals.uran.ua/geofizicheskiy/article/view/111016 |
| work_keys_str_mv | AT kutasri thermalflowandgeothermicmodelsoftheearthscrustoftheukrainiancarpathians |