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Crustal recycling and metamorphic dehydration govern the fertility of granite-associated tin systems
Abstract Tin is a critical metal predominantly sourced from granite-associated deposits linked to anatexis of metasedimentary rocks and extreme magmatic differentiation. However, how metamorphism of sedimentary protoliths prior to crustal melting influences granite Sn fertility remains poorly constrained. Here we present an integrated boron (B) and mercury (Hg) isotope study of granites, metasedimentary basement rocks, and ores from the western Yunnan segment of the Southeast Asian Tin Belt.
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