Geology, Mineralogy, Fluid Inclusion, and H–O–S–Pb Isotope Constraints on Ore Genesis of the Keyue Sb–Pb–Zn–Ag Deposit in Southern Tibet

Figure 12

Diagram of Zn/Cd ratios versus Cd for sphalerite from the Keyue Sb–Pb–Zn–Ag deposit, compared with the Zhaxikang deposit (data cited from [9, 20]), as well as high-temperature (porphyry, magmatic hydrothermal, skarn, and VMS-type Pb–Zn deposit), low-temperature (MVT deposits), and exhalative systems (SEDEX-type Pb–Zn deposits and the seafloor hydrothermal sulfides; data cited from Wen et al. [59]).