The possible nature of the seismic activity of the depths of the Predobudruzhsky trough and the Northern Dobruja
PeriDobruzha depression and its surrounding belong to border zone of the mantle under the EEP, distinguished by the changes of zero isoline of velocity discrepancies with the depth within the limits of the upper mantle and its transition zone according to the data of 3D P-velocity model. The system...
Збережено в:
| Дата: | 2013 |
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| Автори: | , , , , , , |
| Формат: | Стаття |
| Мова: | rus |
| Опубліковано: |
Subbotin Institute of Geophysics of the NAS of Ukraine
2013
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| Онлайн доступ: | https://journals.uran.ua/geofizicheskiy/article/view/116331 |
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| Назва журналу: | Geofizicheskiy Zhurnal |