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Laura Rzehak-Wissink, Sebastian Kommescher, Florian Kurzweil, Peter Sprung, Felipe Padilha Leitzke, Raúl O.C. Fonseca

• Equilibria between Ti oxides and silicate melt lead to Ti isotope fractionation in terrestrial samples, with isotopically light Ti oxides and isotopically heavy coexisting melt. However, while Ti is mostly tetravalent in terrestrial samples, around 10% of the overall Ti is trivalent at \(\it fO_{2}\) relevant to lunar magmatism (~ IW-1). The different valences of Ti in lunar samples, could additionally influence Ti stable isotope fractionation during petrogenesis of lunar basalts to an unknown extent. We performed an experimental approach using gas mixing furnaces to investigate the effect of Ti oxide formation at different \(\it fO_{2}\) on Ti stable isotope fractionation during mare basalt petrogenesis. Two identical bulk compositions were equilibrated simultaneously during each experiment to guarantee comparability. One experiment was investigated with the EPMA to characterize the petrology of experimental run products, whereas the second experiment was crushed, and fabricated phases (i.e., oxides, silicates and glass) were handpicked, separated and digested. An aliquot of each sample was mixed with a Ti double-spike, before Ti was separated from matrix and interfering elements using a modified HFSE chemistry. Our study shows \(\it fO_{2}\)-dependent fractionation within seven samples from air to IW-1, especially \(\Delta^{49}Ti_{armalcolite-melt}\) and \(\Delta^{49}Ti_{armalcolite-orthopyroxene }\)become more fractionated from oxidized to reduced conditions (− 0.092 \(\pm\) 0.028-  − 0.200 \(\pm\) 0.033 ‰ and  − 0.089 \(\pm\) 0.027- − 0.250 \(\pm\) 0.049 ‰, respectively), whereas \(\Delta^{49}Ti_{orthopyroxene-melt}\) shows only a minor fractionation (− 0.002 \(\pm\) 0.017-0.050 \(\pm\) 0.025 ‰). The results of this study show that Ti isotope fractionation during mare basalt petrogenesis is expected to be redox dependent and mineral-melt fractionation as commonly determined for terrestrial \(\it fO_{2}\) may not be directly applied to a lunar setting. This is important for the evaluation of Ti isotope fractionation resulting from lunar magmatism, which takes place under more reducing conditions compared to the more oxidized terrestrial magmatism.