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Tin granite, Protolith composition, Pre-enrichment, Metasediment, Thermodynamic modeling, South China
Abstract:
Important features of Sn mineralization are the heterogeneous geographic distribution and frequent regional
separation from W mineralization in spite some similarities of Sn and W behavior during magmatic processes.
Major Sn and W mineralization is often spatially associated with peraluminous granites, which are derived from
partial melting of metasediments. Several concepts have been suggested to explain those features, such as a
weathering-related Sn-enriched source, Sn redistribution between melts and restite during protolith melting, and
extensive fractional crystallization. We demonstrate the importance of protolith composition for the formation of Sn (and W) granites by using a comprehensive bulk-rock composition dataset from Precambrian metasediments
of the South China Sn-W province and employing a thermodynamic modeling approach. We used four compositional
proxies for phase equilibria calculations, which are the metasediments of the Mengdong, Sibao, Pingbian, and Shuangqiaoshan Groups. It is well documented that those Precambrian metasediments are important protoliths of Sn granites in South China. We present quantitative evaluation of the control of protolith composition in the generation of Sn-enriched granitic melts using South China as example, but our conclusions may also be applicable to worldwide Sn–enriched granites. Our results indicate that the protolith major-element geochemistry controls the anatectic reactions and melt productivity at specific melting conditions, and consequently the partitioning behavior of Sn. Further, pre-enrichment of Sn is crucial to the fertility of granitic melt and may be a prerequisite, particularly for the formation of giant Sn deposits. We propose that the heterogeneous distribution of favorable source rocks is one of the important factors that control the spatial distribution of major Sn (and W) districts in South China and other regions worldwide.
