Junction zone of the Dnieper-Donets avlacogen and the Ukrainian crystalline massif
Abstract
According to the latest ideas, the Dnieper-Donets Depression is a transverse avlacogen that arose in the late stages of the Russian Platform development in the Middle Devonian, when not only the platform basement but also a significant part of the platform cover had already been formed...
Область исследования:
(Archived) Without section
References
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