Geoelectric studies of the Belgorod-Sumy megablock of the northern slope of the Dnieper-Donets Trough
Processing of long-term Earth’s electromagnetic field observations was performed using two software systems (PRC_MTMV and PTS), frequency distribution of the amplitude and phase of impedance, apparent resistivity, horizontal components of the magnetic tensor and tipper were obtained. Minimum on the...
Збережено в:
| Дата: | 2015 |
|---|---|
| Автори: | , , |
| Формат: | Стаття |
| Мова: | Українська |
| Опубліковано: |
S. Subbotin Institute of Geophysics of the NAS of Ukraine
2015
|
| Теми: | |
| Онлайн доступ: | https://journals.uran.ua/geofizicheskiy/article/view/111163 |
| Теги: |
Додати тег
Немає тегів, Будьте першим, хто поставить тег для цього запису!
|
| Назва журналу: | Geofizicheskiy Zhurnal |
Репозитарії
Geofizicheskiy Zhurnal| Резюме: | Processing of long-term Earth’s electromagnetic field observations was performed using two software systems (PRC_MTMV and PTS), frequency distribution of the amplitude and phase of impedance, apparent resistivity, horizontal components of the magnetic tensor and tipper were obtained. Minimum on the descending part of ρk curves according to the results of a qualitative assessment corresponds to the conductor at a depth of 50—150 km. |
|---|