Research Article

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

Table 4

The S isotopic data for sulfides from the Keyue deposit.

Sample numberMineralδ34SCDTDescription

D41-2-4Sp210.6Stage 2 massive sphalerite–galena–chalcopyrite.
Gn28.4

ZK805-H8Sp29.4Stage 2 massive sphalerite–galena–chalcopyrite.
Gn27.4

Zk1604-H25Gn25.4Stage 2 massive sphalerite–galena–Mn–Fe carbonate cut by stage 4 quartz–boulangerite vein.
Sp210.2
Blr46.6

D41-3-1Sp211.2Stage 2 massive sphalerite cut by stage 4 quartz–boulangerite vein.
Blr49.9

D39-4-2Sp211.2Stage 2 massive sphalerite cut by stage 4 quartz–boulangerite vein.
Blr47.4

D40-2Sp311.2Stage 3 massive sphalerite–galena–chalcopyrite–galena; there are minor amounts of Mn–Fe carbonate left.
Gn37.4

D39-5-2Gn34.9Stage 3 massive sphalerite–galena–chalcopyrite cross-cut by quartz veins.
Ccp36.4

D40-1-2Sp37.1Stage 3 quartz–sphalerite.

D41-5Sp39.6Stage 3 massive quartz–sphalerite–chalcopyrite cut by stage 4 quartz–boulangerite vein.
Ccp37.0

ZK003-433-1Sp39.9Stage 3 sphalerite–calcite

D41-8Py36.6Stage 3 pyrite occurs in quartz; there are minor amounts of Mn–Fe carbonate left.

D41-7-1 (3)Py35.0Stage 3 quartz–pyrite–galena vein cut the Mn-Fe carbonate.

KY-1-1Stb58.2Stage 5 radial stibnite occurs in stage 5 quartz.

Note: Sp2 = stage 2 sphalerite; Gn2 = stage 2 galena; Sp3 = stage 3 sphalerite; Gn3 = stage 3 galena; Ccp3 = stage 3 chalcopyrite; Py3 = stage 3 pyrite; Blr4 = stage 4 boulangerite; Stb5 = stage 5 stibnite.