Моделирование фоновых температурных полей ДДВ
Using facts of rifting origin and development of Dneprovsko-Donetsky hollow (DDH), it was carried out computer modeling of the phone temperature fields of the earth crust in the cross sections of Chernigov, Poltava and Harkov megablocks of DDH. It was showed, that visible distinctions of the tempera...
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| Опубліковано в: : | Геодинаміка |
|---|---|
| Дата: | 2009 |
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| Формат: | Стаття |
| Мова: | Російська |
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Інститут геофізики ім. С.I. Субботіна НАН України
2009
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| Онлайн доступ: | https://nasplib.isofts.kiev.ua/handle/123456789/18543 |
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| Назва журналу: | Digital Library of Periodicals of National Academy of Sciences of Ukraine |
| Цитувати: | Моделирование фоновых температурных полей ДДВ / M.В. Лубков // Геодинаміка. — 2009. — № 1(8). — С. 91-96. — Бібліогр.: 13 назв. — рос. |
Репозитарії
Digital Library of Periodicals of National Academy of Sciences of Ukraine| _version_ | 1860045296778608640 |
|---|---|
| author | Лубков, М.В. |
| author_facet | Лубков, М.В. |
| citation_txt | Моделирование фоновых температурных полей ДДВ / M.В. Лубков // Геодинаміка. — 2009. — № 1(8). — С. 91-96. — Бібліогр.: 13 назв. — рос. |
| collection | DSpace DC |
| container_title | Геодинаміка |
| description | Using facts of rifting origin and development of Dneprovsko-Donetsky hollow (DDH), it was carried out computer modeling of the phone temperature fields of the earth crust in the cross sections of Chernigov, Poltava and Harkov megablocks of DDH. It was showed, that visible distinctions of the temperature fields were fixed in the lower and middle parts of the crust, in the upper part, starting from 10 km layer, temperature fields were differed very little. Also the contribution of radioactivity, from 6 km layer consisted of approximately a third part of the near surface common phone temperature field. The temperature conditions in basalt layers of the lower crust demonstrated increasing of probability of the forming derivatives of eclogite metamorphism in the southeast direction. The comparison of the obtained results with the temperature measurements data in the upper crust part supports rifting origin theory of DDH.
|
| first_indexed | 2025-12-07T16:58:11Z |
| format | Article |
| fulltext |
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MODELING OF THE PHONE TEMPERATURE FIELDS OF DDH
M.V. Lubkov
Using facts of rifting origin and development of Dneprovsko-Donetsky hollow (DDH), it was carried out
computer modeling of the phone temperature fields of the earth crust in the cross sections of Chernigov, Poltava
and Harkov megablocks of DDH. It was showed, that visible distinctions of the temperature fields were fixed in
the lower and middle parts of the crust, in the upper part, starting from 10 km layer, temperature fields were
differed very little. Also the contribution of radioactivity, from 6 km layer consisted of approximately a third part
of the near surface common phone temperature field. The temperature conditions in basalt layers of the lower
crust demonstrated increasing of probability of the forming derivatives of eclogite metamorphism in the south-
east direction. The comparison of the obtained results with the temperature measurements data in the upper crust
part supports rifting origin theory of DDH
Key words: Dneprovsko-Donetsky hollow; rifting; astenolite; heat fields; computer modeling.
. . . , .
07.10.2008
|
| id | nasplib_isofts_kiev_ua-123456789-18543 |
| institution | Digital Library of Periodicals of National Academy of Sciences of Ukraine |
| issn | 1992-142X |
| language | Russian |
| last_indexed | 2025-12-07T16:58:11Z |
| publishDate | 2009 |
| publisher | Інститут геофізики ім. С.I. Субботіна НАН України |
| record_format | dspace |
| spelling | Лубков, М.В. 2011-04-01T07:38:27Z 2011-04-01T07:38:27Z 2009 Моделирование фоновых температурных полей ДДВ / M.В. Лубков // Геодинаміка. — 2009. — № 1(8). — С. 91-96. — Бібліогр.: 13 назв. — рос. 1992-142X https://nasplib.isofts.kiev.ua/handle/123456789/18543 550.36 Using facts of rifting origin and development of Dneprovsko-Donetsky hollow (DDH), it was carried out computer modeling of the phone temperature fields of the earth crust in the cross sections of Chernigov, Poltava and Harkov megablocks of DDH. It was showed, that visible distinctions of the temperature fields were fixed in the lower and middle parts of the crust, in the upper part, starting from 10 km layer, temperature fields were differed very little. Also the contribution of radioactivity, from 6 km layer consisted of approximately a third part of the near surface common phone temperature field. The temperature conditions in basalt layers of the lower crust demonstrated increasing of probability of the forming derivatives of eclogite metamorphism in the southeast direction. The comparison of the obtained results with the temperature measurements data in the upper crust part supports rifting origin theory of DDH. ru Інститут геофізики ім. С.I. Субботіна НАН України Геодинаміка Геофізика Моделирование фоновых температурных полей ДДВ Моделювання фонових температурних полів ДДЗ Modeling of the phone temperature fields of DDH Article published earlier |
| spellingShingle | Моделирование фоновых температурных полей ДДВ Лубков, М.В. Геофізика |
| title | Моделирование фоновых температурных полей ДДВ |
| title_alt | Моделювання фонових температурних полів ДДЗ Modeling of the phone temperature fields of DDH |
| title_full | Моделирование фоновых температурных полей ДДВ |
| title_fullStr | Моделирование фоновых температурных полей ДДВ |
| title_full_unstemmed | Моделирование фоновых температурных полей ДДВ |
| title_short | Моделирование фоновых температурных полей ДДВ |
| title_sort | моделирование фоновых температурных полей ддв |
| topic | Геофізика |
| topic_facet | Геофізика |
| url | https://nasplib.isofts.kiev.ua/handle/123456789/18543 |
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