“…This coherence is absent during aqueous processes due to the different grades of Zr and Hf hydrolysis and dissolved complexation in natural waters (Aja et al, 1995;Veyland et al, 1998;Byrne, 2002;Hagfeldt et al, 2004;Messner et al, 2011a;2011b;Inguaggiato et al, 2015Inguaggiato et al, , 2016Censi et al, 2017). Aqueous environments usually make Hf more surface-reactive than Zr, which changes the associated Zr/Hf with respect to the range of values recognised in rocks and minerals and provides a useful signature of solid-liquid processes.…”