Genesis of the Zhijiadi Ag-Pb-Zn Deposit, Central North China Craton: Constraints from Fluid Inclusions and Stable Isotope Data

Table 3

Sulfur isotope data of sulfide minerals from the Zhijiadi Ag-Pb-Zn deposit.

Number	Sample ID	Description	Mineral	()
(1)	16ZJD-28	Massive	Py
			Py
			Py
			Py
			Py
			Sp
			Sp
			Sp
			Sp
			Sp
			Sp
			Sp
			Ccp
			Ccp
			Gn
			Gn
			Gn
			Gn
			Gn
			Gn
			Gn
			Gn
			Gn
			Gn
			Gn
			Gn
			Gn
(2)	16ZJD-29	Stockwork	Py
			Py
			Py
			Py
			Py
			Py
			Py
			Py
			Py
			Py
			Py
			Py
			Gn
(3)	16ZJD-31	Massive	Gn
			Gn
			Gn
			Gn
			Gn
			Gn
			Gn
(4)	16ZJD-38	Veinlet-disseminated	Py
			Py
			Py
			Sp
			Gn
(5)	ZK2207-36	Granite porphyry	Py
			Py
			Py
(6)	ZK2207-89	Veinlet-disseminated	Py
			Sp
			Py
			Sp
(7)	16ZJD-2	Stockwork	Py
			Py
			Gn
			Gn
			Gn
			Sp
			Gn
(8)	16ZJD-6	Vein	Sp
			Gn
			Sp
			Gn
(9)	16ZJD-7	Brecciated	Py
			Py
			Py
			Py
			Py
			Py
			Py
			Py
			Sp
			Sp
			Sp
			Sp
			Gn
			Py
			Gn
(10)	16ZJD-17	Stockwork	Py
			Py
			Sp
			Sp
			Sp
			Gn
			Gn
(11)	16ZJD-13	Vein	Gn
			Gn
			Gn
			Py
			Gn
			Gn
			Gn
			Gn
	16ZJD-18	Massive	Py
			Py
			Sp
			Sp
			Sp
			Gn
			Gn
			Gn
			Py
			Sp
(12)	16ZJD-23	Stockwork	Py
			Py
			Sp
			Ccp
			Gn
(13)	16ZJD-27	Stockwork	Py
			Py
			Gn

Note. The sulfur isotope equilibrium temperatures of mineral pair (sphalerite and galena) are calculated using the equilibrium fractionation equation [39]. In the sample 16ZJD-2, the sulfur isotope equilibrium temperature is estimated to be 237°C from mineral pair of sphalerite () and galena (), while it is 267°C from mineral pair of sphalerite () and galena () in the sample 16ZJD-6. As a whole, the temperatures vary from 237 to 267°C. Py, pyrite; Sp, sphalerite; Gn, galena; Ccp, chalcopyrite.