“…Fe-Ti oxides (rutile, ilmenite, titanomagnetite, ulvospinel or magnetite) are common accessory minerals in many metamorphic, magmatic and also detrital rocks. Rodingites are no exception and often contain minor amounts of these phases, mainly rutile and ilmenite (Butek et al, 2022;Koutsovitis et al, 2018Koutsovitis et al, , 2013Laborda-López et al, 2018;Nishiyama et al, 2017). Any attempt to date the metasomatic process with rutile U-Pb geochronology requires a good understanding of 1) the relationship between fluid circulation and Fe-Ti oxide phase equilibria and 2) behaviour of the chemical and isotopic systems during and after mineral crystallization.…”