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Assembly of the Lhasa and Qiangtang terranes in central Tibet by divergent double subduction
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文摘

Two magmatic arcs on the opposing overriding Lhasa and Qiangtang terranes

Extensive 120–110 Ma magmatism with enhanced mantle contributions

Absence of Early Cretaceous high-grade metamorphic rocks

Divergent double-sided subduction of the Bangong oceanic lithosphere

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