Genesis of the Longmendian Ag–Pb–Zn Deposit in Henan (Central China): Constraints from Fluid Inclusions and H–C–O–S–Pb Isotopes

Table 1

Microthermometric data of W-type FIs from quartz in the Longmendian Ag-Pb-Zn deposit.

Stage	Minerals	FI type	Tmice (°C)	Thtot (°C)	Salinity (wt% NaCleqv)
1	Quartz	W	-9.4 to -2.4	198 to 332 (L)	4.0 to 13.3
2	Quartz	W	-9.2 to -0.6	132 to 260 (L,V)	1.1 to 4.3; 6.6 to 13.1
3	Quartz	W	-4.8 to -1.1	97 to 166 (L)	1.9 to 7.6

Tmice: final melting temperature; Thtot: total homogenization temperature. L and V mean that the FIs homogenized to liquid (L) or vapor (V).