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Early Paleozoic felsic magmatic evolution of the western Central Qilian belt, Northwestern China, and constraints on convergent margin processes
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文摘
Oceanic subduction to post-orogenic collapse in Paleozoic Central Qilian c. 465 to 445 Ma stage of post-collisional slab-detachment and mantle upwelling Post-collisional processes contribute greatly to crustal growth.

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