Fluid Inclusion and Oxygen Isotope Constraints on the Origin and Hydrothermal Evolution of the Haisugou Porphyry Mo Deposit in the Northern Xilamulun District, NE China

Figure 7

Homogenization temperature versus salinity plot of fluid inclusion assemblages (in color). Error bars are at 1 level. Individual fluid inclusion analyses in each assemblage are also plotted in black and white. P-, S-, and B-stage refer to pre-, syn-, and postmineralization stage, respectively.