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Contrasting crustal evolution processes in the Dharwar craton: Insights from detrital zircon U-Pb and Hf isotopes
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文摘

Terrane accumulation in the Dharwar craton began ~ 3 Ga in older Western block.

Final cratonisation at 2.5 Ga is much later than other Archaean cratons.

Tectonic, not genetic, links with the Kaapvaal and north China cratons.

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