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Coevolution between crustal thickness and sulfur oxidation state in Gangdese felsic magmas
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DOI：10.1016/j.epsl.2026.120220.png)
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Abstract
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• Detrital records reveal orogen-scale evolution of magmatic S oxidation state. • Magmatic S oxidation state coevolves with crustal thickness. • Detrital zircon-hosted apatite provides a proxy for regional porphyry-Cu potential.
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5.1
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774
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6.9W
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