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Various lines of evidence suggest that they originally crystallized from magmas with roughly andesitic compositions, which some geochemists suggest to have formed the first continental crust (see Much of the “new” archean crust formed during this period comprised a very distinct association of three types of granitoid rocks — tonalite, trondhjemite and granodiorite (ttg). Zircons and early continents no longer to be sneezed at

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Tonalite, trondhjemite, and granodiorite were the first continental rocks and continue to make up large parts of canada among other places 4 ga means that eoarchean oceanic crust, analogous to oceanic plateau crust, was the dominant surface rock type and a likely protolith from which the ettg originated. The first continents emerged about 3.5 billion years.

The building blocks of the first continents are comprised of three types of granitoid rocks—tonalite, trondhjemite and granodiorite (ttg)

Once the oceans cooled and developed on earth, that was almost all that was there. Identifying the building blocks of earth’s early crust, particularly the formation of ttg rocks during the archean eon, has been challenging for scientists studying continental formation. The building blocks of the first continents are comprised of three types of granitoid rocks—tonalite, trondhjemite and granodiorite (ttg). New research suggests that earth's first crust, formed over 4.5 billion years ago, already carried the chemical traits we associate with modern continents

The lack of continental crust at ca