“…In addition, generations of matrix and fracture-fill minerals may also contain some sort of geochemical record (e.g. O, C, Sr isotopes) of the compositions of the groundwaters from which they precipitated (Clauer et al, 1989;Stuckless et al, 1991;Marshall et al, 1992;Gao et al, 1992;Tullborg et al, 2008;Drake and Tullborg, 2009). Isotope tracers are useful tools for deciphering the origin of fluids and diagenetic conditions (Suchy et al, 2000;Morad et al, 2010); fluids and hydrothermal systems (Hecht et al, 1999;Barker et al, 2009;Staude et al, 2011) and deep fluid processes in fault systems (Kopf et al, 2003;Boiron et al, 2003).…”