Origin and Evolution of the Ore-Forming Fluids in the Liyuan Gold Deposit, Central North China Craton: Constraints from Fluid Inclusions and H-O-C Isotopic Compositions

Figure 8

Histograms of total homogenization temperatures () and salinities of C-type and W-type fluid inclusions in the early stage (a, b), middle stage (c, d), and W-type fluid inclusions in the late stage (e, f).

(a)

(b)

(c)

(d)

(e)

(f)