Donbas geoelectrical structure
The Donbas was formed as the result of Late Devonian rifting of the East European craton. During the Carboniferous, the subsidence of the basin and sedimentation were at their maximum, and a 15-kilometer stratum of Carboniferous deposits formed in the Donbas. The total thickness of the deposits rea...
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| Автори: | , |
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| Формат: | Artigo |
| Мова: | Inglês |
| Опубліковано: |
Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine
2022-04-01
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| Серія: | Геофизический журнал |
| Предмети: | |
| Онлайн доступ: | https://journals.uran.ua/geofizicheskiy/article/view/253717 |
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