Heavy silicon isotope and mass-independent mercury isotope fractionation signals of Archean TTGs: Insights into the recycling of the silicified oceanic crust in the source region
Published: 6 March 2026| Version 1 | DOI: 10.17632/ssg8wy4xmw.1
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xiao huDescription
Data for Figure 3, Figure 6a, Figure 6b, and Figure 8 of the article "Heavy silicon isotope and mass-independent mercury isotope fractionation signals of Archean TTGs: Insights into the recycling of the silicified oceanic crust in the source region".
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Geochemistry, Isotope