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Different proportion of mantle-derived noble gases in the Cu-Fe and Fe skarn deposits: He-Ar isotopic constraint in the Edong district, Eastern China
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He–Ar isotopic compositions are markedly different between the Cu–Fe and Fe skarns.

Noble gas within these Cu–Fe and Fe skarns were derived from mixture between magmatic fluid and MASW.

Different proportion of mantle-derived noble gases between the Cu–Fe and Fe skarns

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