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Geological Formation

Yilgarn Craton

Structural and Tectonic Formations

The Yilgarn Craton is a large craton that forms a major part of the Western Australian landmass, bounded by a mix of sedimentary basins and Proterozoic fold and thrust belts. Zircon grains from the Jack Hills, in the craton's Narryer terrane, have been dated to about 4.27 billion years old, with one detrital zircon dated as old as 4.4 billion years, among the oldest known material on Earth. Its Murchison Province also contains the Yarrabubba impact structure, dated at over 2 billion years old, and evidence has been reported of an even older impact crater roughly 3.47 billion years old.

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: Yilgarn Craton

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: Yilgarn Craton
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Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Yilgarn Craton
Sources
Wikidata: Yilgarn Craton
Wikidata Q8053599, class allow-list match (w-wdresolver-0926)View the Source
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