Subcidence patterns (rate of evolution) of Moscow basin
- Авторлар: Dolginov EA1, Lafi G1
-
Мекемелер:
- Peoples’ Friendship University of Russia
- Шығарылым: № 2 (2013)
- Беттер: 45-49
- Бөлім: Articles
- URL: https://journals.rcsi.science/2312-8143/article/view/335616
- ID: 335616
Дәйексөз келтіру
Аннотация
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.
Негізгі сөздер
Авторлар туралы
E Dolginov
Peoples’ Friendship University of RussiaEngineering Faculty
G Lafi
Peoples’ Friendship University of RussiaEngineering Faculty
Қосымша файлдар
