The high-speed structure of the upper floors of the mantle of the Black Sea basin
Lateral velocity variations in the mantle lithosphere of the Black Sea basin down to the depth of 80 km were estimated from travel time residuals of P-waves recorded at the coastal stations from earthquakes within and around the Black Sea. The observed data were corrected for the crust structure tha...
Збережено в:
| Дата: | 2011 |
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| Автори: | , |
| Формат: | Стаття |
| Мова: | rus |
| Опубліковано: |
Subbotin Institute of Geophysics of the NAS of Ukraine
2011
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| Онлайн доступ: | https://journals.uran.ua/geofizicheskiy/article/view/116929 |
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| Назва журналу: | Geofizicheskiy Zhurnal |