“…The inverse linear trend between Nd and Sr isotope compositions reflects the general relationship present in crustal rocks and materials (Allègre, 2008; Allègre et al., 1979; DePaolo, 1988). Consequently, in most situations, ε Nd values are also negatively correlated with Sr isotope ratios in juvenile and hydrothermal waters (Cui et al., 2020; Jakubowicz et al., 2019, 2020; Négrel et al., 2000) and groundwaters (e.g., Nakano, 2016; Négrel & Petelet‐Giraud, 2010; Tricca et al., 1999).…”