HAL (France)
open access
Copper isotope evidence for Cu transfer during oceanic crust subduction: insights from the (ultra)high-pressure metamorphic belt of Southwestern Tianshan, China
Constraining the behavior of Cu during subduction is the key to decipher processes leading to the porphyry Cu deposit formation at convergent margins, while also shedding light on S cycling owing to the chalcophile affinity of Cu. This study reported δ65Cu values for bulk-rock and chalcop
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