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Petrogenesis of middle Ordovician peraluminous granites in the Baoshan block: Implications for the early Paleozoic tectonic evolution along East Gondwana
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文摘

Crustal anatexis produces ca. 470–460 Ma peraluminous granites.

Lithospheric delamination occurs following final Asian continental accretion.

Slab breakoff and lithosphere delamination drive most ca. 500–450 Ma granites.

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