Earth and Environment Atlas

How The Planet Works
Sign In
Text size
100%
Theme
Geological Formation

Ukrainian Shield

Structural and Tectonic Formations

The Ukrainian Shield, also called the Ukrainian Crystalline Massif, is the southwestern shield of the East European Craton, covering an area of about 200,000 square kilometers over a stretch roughly 1,000 kilometers long and up to 250 kilometers wide. Its rock is ancient, combining Archean crust between 3.2 and 3.8 billion years old in its southwestern and eastern portions with Early Proterozoic orogenic belts dated to between 2.1 and 2.3 billion years old, and it is recognized as a major pegmatite province divided into seven megastructures, each with its own distinct mineralogy and geochemistry. As part of the East European Craton, a stable ancient continental platform, it shares close geological ties with the neighboring Voronezh Massif to the east, and the Ilyinets impact crater lies along the boundary between two of its megastructures, the Rosynsko-Tikychki and Dnistersko-Buzki zones.

Connections

Caused By

Wikidata P31 formation-type mapped to formative process Plate Tectonics via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Ukrainian Shield

In Discipline

Wikidata P31 formation-type mapped to discipline Structural Geology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Ukrainian Shield
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Ukrainian Shield

Also in Geography Atlas: where this subject is found.

Source Wikidata: Ukrainian Shield

Also in Geography Atlas: where this subject is found.

Source Wikidata: Ukrainian Shield
Sources
Wikidata: Ukrainian Shield
Wikidata Q521551, class allow-list match (w-wdresolver-0926)View the Source
Comments (0)
No comments yet. Be the first to share a thought.
Reader Challenges (0)
No disputes yet. Spotted an error or a better source? Open the first one.