Comparison of geophysical sections of the Earth crust with the results of deep drilling in the Fennoscandian Shield
The nature of geoacoustic waves is discussed, based on comparison of the results of seismic and acoustic studies in the Fennoscandian Shield with the drilling record of the Kola Superdeep Borehole: 12262 m (1970-1990), Russia; Gravberg 6337 m (1986-1987), Sweden; Outokumpu - 2516 m (2004-2005), Finl...
Збережено в:
| Дата: | 2012 |
|---|---|
| Автор: | |
| Формат: | Стаття |
| Мова: | rus |
| Опубліковано: |
Subbotin Institute of Geophysics of the NAS of Ukraine
2012
|
| Онлайн доступ: | https://journals.uran.ua/geofizicheskiy/article/view/116779 |
| Теги: |
Додати тег
Немає тегів, Будьте першим, хто поставить тег для цього запису!
|
| Назва журналу: | Geofizicheskiy Zhurnal |
Репозитарії
Geofizicheskiy Zhurnal| id |
journalsuranua-geofizicheskiy-article-116779 |
|---|---|
| record_format |
ojs |
| spelling |
journalsuranua-geofizicheskiy-article-1167792020-10-07T12:21:33Z Comparison of geophysical sections of the Earth crust with the results of deep drilling in the Fennoscandian Shield Sharov, N. V. The nature of geoacoustic waves is discussed, based on comparison of the results of seismic and acoustic studies in the Fennoscandian Shield with the drilling record of the Kola Superdeep Borehole: 12262 m (1970-1990), Russia; Gravberg 6337 m (1986-1987), Sweden; Outokumpu - 2516 m (2004-2005), Finland; Pogranichnaya - 5200 m (2004-2006), Russia; Onezhskaya - 3537 m (2007-2009), Russia. The assumption that the crystalline crust has a heterogeneous structure with gradient variations and elastic wave velocity inversions and the vertically and laterally varying degree of differentiation is wellbased. The nature of seismic boundaries depends on differences in rock composition and the physical state of the rocks. The results of geophysical studies, conducted during deep drilling in the Fennoscandian Shield, make investigators reinterpret the geological and geophysical data. Subbotin Institute of Geophysics of the NAS of Ukraine 2012-08-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116779 10.24028/gzh.0203-3100.v34i4.2012.116779 Geofizicheskiy Zhurnal; Vol. 34 No. 4 (2012); 253-264 Геофизический журнал; Том 34 № 4 (2012); 253-264 Геофізичний журнал; Том 34 № 4 (2012); 253-264 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/116779/110836 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| institution |
Geofizicheskiy Zhurnal |
| collection |
OJS |
| language |
rus |
| format |
Article |
| author |
Sharov, N. V. |
| spellingShingle |
Sharov, N. V. Comparison of geophysical sections of the Earth crust with the results of deep drilling in the Fennoscandian Shield |
| author_facet |
Sharov, N. V. |
| author_sort |
Sharov, N. V. |
| title |
Comparison of geophysical sections of the Earth crust with the results of deep drilling in the Fennoscandian Shield |
| title_short |
Comparison of geophysical sections of the Earth crust with the results of deep drilling in the Fennoscandian Shield |
| title_full |
Comparison of geophysical sections of the Earth crust with the results of deep drilling in the Fennoscandian Shield |
| title_fullStr |
Comparison of geophysical sections of the Earth crust with the results of deep drilling in the Fennoscandian Shield |
| title_full_unstemmed |
Comparison of geophysical sections of the Earth crust with the results of deep drilling in the Fennoscandian Shield |
| title_sort |
comparison of geophysical sections of the earth crust with the results of deep drilling in the fennoscandian shield |
| description |
The nature of geoacoustic waves is discussed, based on comparison of the results of seismic and acoustic studies in the Fennoscandian Shield with the drilling record of the Kola Superdeep Borehole: 12262 m (1970-1990), Russia; Gravberg 6337 m (1986-1987), Sweden; Outokumpu - 2516 m (2004-2005), Finland; Pogranichnaya - 5200 m (2004-2006), Russia; Onezhskaya - 3537 m (2007-2009), Russia. The assumption that the crystalline crust has a heterogeneous structure with gradient variations and elastic wave velocity inversions and the vertically and laterally varying degree of differentiation is wellbased. The nature of seismic boundaries depends on differences in rock composition and the physical state of the rocks. The results of geophysical studies, conducted during deep drilling in the Fennoscandian Shield, make investigators reinterpret the geological and geophysical data. |
| publisher |
Subbotin Institute of Geophysics of the NAS of Ukraine |
| publishDate |
2012 |
| url |
https://journals.uran.ua/geofizicheskiy/article/view/116779 |
| work_keys_str_mv |
AT sharovnv comparisonofgeophysicalsectionsoftheearthcrustwiththeresultsofdeepdrillinginthefennoscandianshield |
| first_indexed |
2024-04-21T19:41:21Z |
| last_indexed |
2024-04-21T19:41:21Z |
| _version_ |
1796974557014261760 |