Subcidence patterns (rate of evolution) of Moscow basin
- Authors: Dolginov EA1, Lafi G1
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Affiliations:
- Peoples’ Friendship University of Russia
- Issue: No 2 (2013)
- Pages: 45-49
- Section: Articles
- URL: https://journals.rcsi.science/2312-8143/article/view/335616
- ID: 335616
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Abstract
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.
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About the authors
E A Dolginov
Peoples’ Friendship University of RussiaEngineering Faculty
G Lafi
Peoples’ Friendship University of RussiaEngineering Faculty
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