Fig. 9From: Geochemical and H–O–Sr–B isotope signatures of Yangyi geothermal fields: implications for the evolution of thermal fluids in fracture-controlled type geothermal system, Tibet, ChinaDiagram of Na vs. Cl, SO4 vs. Cl, vs. Cl, B vs. Cl, Ca vs. Cl and Mg vs. Cl for the water samples in YHGFBack to article page