Copper-iron Isotopic Fractionation During Formation of Magmatic Sulfide Deposit: Insight from Giant Kalatongke deposit in the Central Asian Orogenic Belt
Published: 23 September 2022| Version 1 | DOI: 10.17632/7gnc86dwhk.1
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Dongmei TangDescription
Table S1-S4 for Dongmei Tang
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Institutions
Institute of Geology and Geophysics Chinese Academy of Sciences
Categories
Sulfide, Mineral Deposit, Non-Traditional Isotope Geochemistry