Jump to content

Volgo–Uralia

From Wikipedia, the free encyclopedia

This is the current revision of this page, as edited by Altenmann (talk | contribs) at 06:51, 23 November 2023. The present address (URL) is a permanent link to this version.

(diff) ← Previous revision | Latest revision (diff) | Newer revision → (diff)

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

[edit]
  1. ^ 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.