Deep seated structure of the Dnieper-Donets paleorift in the system of the Sarmat-Turanian lineament
© Trypolskiy O.A., Kalyuzhnaya L.T.
Based upon the results of deep seismic studies the Dnieper-Donets paleorift is shown to be an active rift zone while the adjacent Pripyat depression and Karpinsky bank are the passive rift zones. <<back |
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