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

<div><i>δ</i>D vs <i>δ</i><sup>18</sup>O plot of the ore-forming fluids in the Liyuan gold deposit. Also shown are the isotopic fields for common metamorphic and primary magmatic water [<a href="/journals/geofluids/2017/3107280/#B123">30</a>]. The field for orogenic gold deposit revised after Goldfarb et al. [<a href="/journals/geofluids/2017/3107280/#B124">31</a>].</div>

Geofluids

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Figure 12

Figure 12: 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 12 | 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 