Thermal field of the Donbas
We estimate results of the study of deep heat flow of Donbas. Anomalies of different nature have been distinguished. Their interpretation has been conducted. The thermal model of the crust and upper mantle has been plotted.Self-constructed electrical thermometers have been applied. It was also shown...
Gespeichert in:
| Datum: | 2015 |
|---|---|
| Hauptverfasser: | , , |
| Format: | Artikel |
| Sprache: | Russisch |
| Veröffentlicht: |
S. Subbotin Institute of Geophysics of the NAS of Ukraine
2015
|
| Schlagworte: | |
| Online Zugang: | https://journals.uran.ua/geofizicheskiy/article/view/111169 |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| Назва журналу: | Geofizicheskiy Zhurnal |
Institution
Geofizicheskiy Zhurnal| _version_ | 1856543156775944192 |
|---|---|
| author | Gordienko, V. Gordienko, I. Zavgorodnyaya, O. |
| author_facet | Gordienko, V. Gordienko, I. Zavgorodnyaya, O. |
| author_sort | Gordienko, V. |
| baseUrl_str | |
| collection | OJS |
| datestamp_date | 2020-10-07T11:37:11Z |
| description | We estimate results of the study of deep heat flow of Donbas. Anomalies of different nature have been distinguished. Their interpretation has been conducted. The thermal model of the crust and upper mantle has been plotted.Self-constructed electrical thermometers have been applied. It was also shown, that the used drilling technology (without washing fluid circulation) and the short time of drilling provided a very short borehole “rest”. Already in several hours after finishing drilling stable bottom borehole T were observed during several 24h terms.The main part of heat flow determinations were made by using the results of the borehole bottom Т measurements made by standard logging thermometers in the geophysical borehole logging . As a rule, the boreholes “rest” was from several hours to several days. Instrumental errors of this operation were repeatedly estimated and made the first tenth of a degree centigrade. The main error is clearly due to Т distortions.The data collected generally enable plotting heat flow HF and interior temperature maps scaled at 1: 2 500 000 — 1: 5 000 000. More detailed maps of the Donbas territory where the network density is well above the average one of the Ukraine have also been shown. The HF and deep temperature data are supplemented with the geothermal resource maps of the Donbas. |
| first_indexed | 2025-07-17T11:05:33Z |
| format | Article |
| id | journalsuranua-geofizicheskiy-article-111169 |
| institution | Geofizicheskiy Zhurnal |
| language | Russian |
| last_indexed | 2025-07-17T11:05:33Z |
| publishDate | 2015 |
| publisher | S. Subbotin Institute of Geophysics of the NAS of Ukraine |
| record_format | ojs |
| spelling | journalsuranua-geofizicheskiy-article-1111692020-10-07T11:37:11Z Thermal field of the Donbas Gordienko, V. Gordienko, I. Zavgorodnyaya, O. heat flow deep temperatures thermal model of tectonosphere We estimate results of the study of deep heat flow of Donbas. Anomalies of different nature have been distinguished. Their interpretation has been conducted. The thermal model of the crust and upper mantle has been plotted.Self-constructed electrical thermometers have been applied. It was also shown, that the used drilling technology (without washing fluid circulation) and the short time of drilling provided a very short borehole “rest”. Already in several hours after finishing drilling stable bottom borehole T were observed during several 24h terms.The main part of heat flow determinations were made by using the results of the borehole bottom Т measurements made by standard logging thermometers in the geophysical borehole logging . As a rule, the boreholes “rest” was from several hours to several days. Instrumental errors of this operation were repeatedly estimated and made the first tenth of a degree centigrade. The main error is clearly due to Т distortions.The data collected generally enable plotting heat flow HF and interior temperature maps scaled at 1: 2 500 000 — 1: 5 000 000. More detailed maps of the Donbas territory where the network density is well above the average one of the Ukraine have also been shown. The HF and deep temperature data are supplemented with the geothermal resource maps of the Donbas. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2015-12-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/111169 10.24028/gzh.0203-3100.v37i6.2015.111169 Geofizicheskiy Zhurnal; Vol. 37 No. 6 (2015); 3-23 Геофизический журнал; Том 37 № 6 (2015); 3-23 Геофізичний журнал; Том 37 № 6 (2015); 3-23 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/111169/106029 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| spellingShingle | heat flow deep temperatures thermal model of tectonosphere Gordienko, V. Gordienko, I. Zavgorodnyaya, O. Thermal field of the Donbas |
| title | Thermal field of the Donbas |
| title_full | Thermal field of the Donbas |
| title_fullStr | Thermal field of the Donbas |
| title_full_unstemmed | Thermal field of the Donbas |
| title_short | Thermal field of the Donbas |
| title_sort | thermal field of the donbas |
| topic | heat flow deep temperatures thermal model of tectonosphere |
| topic_facet | heat flow deep temperatures thermal model of tectonosphere |
| url | https://journals.uran.ua/geofizicheskiy/article/view/111169 |
| work_keys_str_mv | AT gordienkov thermalfieldofthedonbas AT gordienkoi thermalfieldofthedonbas AT zavgorodnyayao thermalfieldofthedonbas |