Fluid Inclusions and H-O-C-S-Pb Isotope Studies of the Xinmin Cu-Au-Ag Polymetallic Deposit in the Qinzhou-Hangzhou Metallogenic Belt, South China: Constraints on Fluid Origin and Evolution

<div>Calculated oxygen and hydrogen isotope compositions of fluids in equilibrium with quartz from the Xinmin deposit. The fields for metamorphic fluids are after [<a href="/journals/geofluids/2021/5171579/#B33">33</a>], magmatic and peraluminous granite fields from [<a href="/journals/geofluids/2021/5171579/#B34">34</a>, <a href="/journals/geofluids/2021/5171579/#B35">35</a>].</div>

Geofluids

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Figure 8: Fluid Inclusions and H-O-C-S-Pb Isotope Studies of the Xinmin Cu-Au-Ag Polymetallic Deposit in the Qinzhou-Hangzhou Metallogenic Belt, South China: Constraints on Fluid Origin and Evolution 

Figure 8 | Fluid Inclusions and H-O-C-S-Pb Isotope Studies of the Xinmin Cu-Au-Ag Polymetallic Deposit in the Qinzhou-Hangzhou Metallogenic Belt, South China: Constraints on Fluid Origin and Evolution 