Subcidence patterns (rate of evolution) of Moscow basin
Moscow basin had subsided in two “half-waves” velocity regime over the time-span: Cambrian (Vendian) — Devonian and carboniferous. Subsidence pattern of this basin in devonian-carboniferous was similar to that of the Dnepr-Donezk rift basin.
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Peoples’ Friendship University of Russia (RUDN University)
2013-12-01
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| Series: | RUDN Journal of Engineering Researches |
| Subjects: | |
| Online Access: | http://journals.rudn.ru/engineering-researches/article/view/4977 |