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Autor:
M. V. Osipova, R. R. Shakirov, A. G. Koshcheev, S. V. Pisarchuk, A. G. Naymushin, O. P. Nesterov
Publikováno v:
Georesursy, Vol 25, Iss 3, Pp 34-39 (2024)
This work is devoted to the peculiarities of sedimentation and geological structure of clinoform deposits of the Yarudeisky megaswell (Western Siberia). The main feature of the clinoforms under consideration is that the sediments are confined to the
Externí odkaz:
https://doaj.org/article/9fd61c9344b64ff39ff239a67a582a87