Volgo–Uralia

Volgo–Uralia is a crustal segment that together with the Sarmatian Craton and the Fennoscandian Craton makes up the East European Craton. ^[1]

6 relations: Continental crust, East European Craton, Fennoscandia, Precambrian Research, Sarmatian Craton, Tectonostratigraphy.

Continental crust

Continental crust is the layer of igneous, sedimentary, and metamorphic rocks that forms the continents and the areas of shallow seabed close to their shores, known as continental shelves.

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The East European Craton (EEC) is the core of the Baltica proto-plate and consists of three crustal regions/segments: Fennoscandia to the northwest, Volgo-Uralia to the east, and Sarmatia to the south.

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Fennoscandia

Fennoscandia (Fennoskandia; Fennoskandien; Fennoskandia; Фенноскандия Fennoskandiya), Fenno-Scandinavia, or the Fennoscandian Peninsula, is the geographical peninsula of the Nordic region comprising the Scandinavian Peninsula, Finland, Karelia, and the Kola Peninsula.

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Precambrian Research

Precambrian Research is a peer-reviewed scientific journal covering the geology of the Earth and its planetary neighbors.

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Sarmatian Craton

The Sarmatian Craton or Sarmatia is the southern segment/region of the East European Craton or Baltica, also known as Scythian Plateau.

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Tectonostratigraphy

In geology, tectonostratigraphy is stratigraphy that refers either to rock sequences in which large-scale layering is caused by the stacking of thrust sheets, or nappes, in areas of thrust tectonics or to the effects of tectonics on lithostratigraphy.

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Redirects here:

Volgo-Uralia.

References

[1] https://en.wikipedia.org/wiki/Volgo–Uralia

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