Under the support of the National Natural Science Foundation of China (Grant No.
The subduction of the oceanic plate carries a large amount of redox-sensitive valence elements such as S, Fe, and C into the interior of the earth, which drives the oxygen cycle between the earth's surface and the deep part, and is crucial to the formation and maintenance of a habitable earth
The redox state of the primary arc magma determines the content of the variable valence element S in the magma, thereby controlling the systematic change of the sulfide-philic element Cu in the magma
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