The Dharwar Craton is an Archean continental craton formed between about 3.6 and 2.5 billion years ago in southern India, considered the oldest part of the Indian peninsula. Research in the 2010s found it separates into three crustal blocks, western, central and eastern, divided by several shear zones and each showing a different history of block collision. Its rock record is dominated by tonalite-trondhjemite-granodiorite gneisses, volcanic-sedimentary greenstone sequences and calc-alkaline granitoids, with the western block preserving the craton's oldest basement rocks in greenstone sequences dated between 3.0 and 3.4 billion years old.
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Source Dharwar Craton (Wikipedia)
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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: Dharwar 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: Dharwar Craton
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Source Wikidata: Dharwar Craton
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Wikidata: Dharwar Craton
Wikidata Q5269412, class allow-list match (w-wdresolver-0926)View the Source Dharwar Craton (Wikipedia)
Associated With: Archean, Lead paragraph
The Dharwar Craton is an Archean continental crust craton formed between 3.6 and 2.5 billion years ago (Ga), which is located in southern India and considered the oldest part of the Indian peninsula.
Associated With: Archean, Lead, age Archean
The Dharwar Craton is an Archean continental crust craton formed between 3.6 and 2.5 billion years ago (Ga), which is located in southern India and considered the oldest part of the Indian peninsula.
Associated With: Gneiss, Lead, rock Gneiss
The lithologies of the Dharwar Craton are mainly TTG (Tonalite-trondhjemite-granodiorite) gneisses, volcanic-sedimentary greenstone sequences and calc-alkaline granitoids.
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