Volgo–Uralia
In today's world, Volgo–Uralia is a relevant topic that has captured the attention of millions of people around the world. Since its emergence, Volgo–Uralia has generated all kinds of opinions and debates, becoming a meeting point for experts and fans. Over the years, it has become a phenomenon that transcends borders and cultures, sparking growing interest in different areas of knowledge. In this article, we will thoroughly explore the impact and importance of Volgo–Uralia, as well as its implications in the current context.
Volgo–Uralia is a crustal segment that, together with the Sarmatian Craton and the Fennoscandian Craton, makes up the East European Craton. Volgo–Uralia is the easternmost of the three segments and borders the Sarmatian Craton to the southwest along the Pachelma aulacogen and the Fennoscandian Craton to the northwest along the Volhyn–Central Russian aulacogen.
References
- ^ Gorbatschev, Roland; Bogdanova, Svetlana (December 1993). "Frontiers in the Baltic Shield". Precambrian Research. 64 (1–4). Elsevier Science Publishers B.V.: 3–21. Bibcode:1993PreR...64....3G. doi:10.1016/0301-9268(93)90066-B. ISSN 0301-9268. Retrieved 22 September 2015.
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