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Seamount subduction drives cyclicity in continental arc magmatism: A record from southeastern Lhasa terrane
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DOI：10.1016/j.gr.2026.06.003.png)
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Abstract
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• Inherited zircons and enriched isotopes record crustal sediment recycling via diapir melting. • Seamount subduction feeds sediment diapirs whose melting drives flare-ups. • Two seamount subduction episodes match two magmatic flare-ups, linking seamounts to magmatic cyclicity.
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