Geofluids / 2017 / Article / Fig 7

Research Article

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 7

Histograms of CO2 melting temperatures () of CO2-bearing fluid inclusions in the early stage (a) and middle stage (c) quartz grains and CO2 homogenization temperature of CO2-bearing fluid inclusions in the early stage (b) and middle stage (d) quartz or calcite grains.
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