An Early Paleozoic collisional event along the northern margin of the Central Tianshan Block: Constraints from geochemistry and geochronology of granitic rocks
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文摘

The adakitic granodiorite of 496 Ma records the Paleo-Tianshan Ocean’s subduction.

The gneissic granite dated at 426 Ma exhibits features of post-orogenic granite.

The Paleo-Tianshan Ocean closed before 426 Ma.

The Carboniferous granodiorite and monzodiorite are VAG of the North Tianshan Ocean.

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