Fluid evolution of the Jiawula Ag–Pb–Zn deposit, Inner Mongolia: mineralogical, fluid inclusion, and stable isotopic evidence

SIMS zircon U–Pb and molybdenite Re–Os geochronology, Hf isotope, and whole-rock geochemistry of the Wunugetushan porphyry Cu–Mo deposit and granitoids in NE China and their geological significance

“…Zhang et al, 2008), and also is an important polymetallic metallogenic belt hosting different types of hydrothermal deposits (Liu et al, 2001;Mao et al, 2003;D.G. Zhai et al, 2009;Wu et al, 2011b, c;Liu et al, 2012;Zhou et al, 2012;D.G. Zhai et al, 2013), mainly including porphyry, skarn, and epithermal ore deposits that are spatially and temporally associated with the Mesozoic felsic magmatism (Zhao and Zhang, 1997;Mao et al, 2003;F.…”

Geochronological and He–Ar–S isotopic constraints on the origin of the Sandaowanzi gold-telluride deposit, northeastern China

“…These deposits include the Erdaogou gold deposit (126 Ma, Pang and Qiu, 1997), Jinchanggouliang gold deposit (122 Ma, Liu et al, 2002), Dong'an gold deposit (107 Ma, Zhang et al, 2010b) and Tuanjiegou gold deposit (105 Ma, Liu et al, 1999). It is very common in NE China that the ages of most epithermal Au deposits are similar to those of porphyry Cu-Mo(-Au) deposits and vein-or skarn-type Pb-Zn-Ag polymetallic deposits (i.e., 130-110 Ma, Sun et al, 2013;Zhai et al, 2013Zhai et al, , 2014a (Fig. 1c).…”

Nakhlak carbonate-hosted Pb(Ag) deposit, Isfahan province, Iran: a geological, mineralogical, geochemical, fluid inclusion, and sulfur isotope study

“…Mixing of ore-forming fluids can play an important role in the origin and formation of large hydrothermal ore deposits (Zhu et al, 2001;Cooke and McPhail, 2001;Fan et al, 2011;Gu et al, 2011;Zhai et al, 2013). The Nakhlak fluid inclusions in dolomite and barite do not show a significant correlation between homogenization temperature and salinity, and scattering of the data points for dolomite and barite showed approximately horizontal (isothermal) trends.…”