Subcidence patterns (rate of evolution) of Moscow basin

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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.

E A Dolginov

Peoples’ Friendship University of Russia

Engineering Faculty

G Lafi

Peoples’ Friendship University of Russia

Engineering Faculty

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Copyright (c) 2013 Долгинов Е.А., Лафи Г.

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