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.[1]
References
- ^ Gorbatschev, Roland; Bogdanova, Svetlana (December 1993). "Frontiers in the Baltic Shield". Precambrian Research. Elsevier Science Publishers B.V. 64 (1–4): 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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This page was last edited on 23 November 2023, at 06:51