Geofluids

Research Article

Identification of Two Types of Metallogenic Fluids in the Ultra-Large Huize Pb–Zn Deposit, SW China

Table 2

H–O isotopic compositions of sphalerite, calcite, and barite in Huize Pb–Zn deposit, SW China.


Numbers	Positions	Objects			Date source

HZ911-10	1^# orebody	Lumpy calcite	8.6	−59.8	a
HZ911-15	1^# orebody	Lumpy calcite	8.8	−52.4
HZQ25	6^# orebody	Lumpy calcite	7.7	−50.2
HZQ40	6^# orebody	Porphyritic calcite	7.9	−55.6
HZQ47	6^# orebody	Lumpy calcite	7.7	−57.9
HZQ55	6^# orebody	Vein calcite	7.9	−54.1
HZQ66	6^# orebody	Lumpy calcite	8.3	−53.9
HZQ77	6^# orebody	Vein calcite	8.0	−58.0
HZQ85	6^# orebody	Porphyritic calcite	7.5	−52.7
HQ10-12	10^# orebody	Lumpy calcite	8.7	−53.2
HQ10-18	10^# orebody	Lumpy calcite	7.0	−57.3
HQ10-25	10^# orebody	Porphyritic calcite	8.1	−53.0
HQ10-5	10^# orebody	Vein calcite	7.4	−52.8
HQ8-115	8^# orebody	Lumpy calcite	7.2	−55.2
HQ8-143	8^# orebody	Lumpy calcite	7.8	−54.1
HQ8-98	8^# orebody	Vein calcite	8.0	−54.3

HQO-99-1	Qilinchang	Calcite	7.8	−43.5	b
HQO-109-4	Qilinchang	Calcite	10.1	−54.8
1631-38	Qilinchang	Calcite	7.8	−48.0
HQ-84	Qilinchang	Calcite	9.7	−51.5
HQ-109-4	Qilinchang	Calcite	7.6	−43.5
1751-2	Qilinchang	Calcite	7.7	−55.4

HW-2-3	Qilinchang	Calcite	7.1	−55.8	c
38-3	Qilinchang	Calcite	6.4	−64.0
Hui-6-10	Qilinchang	Calcite	7.1	−75.0
13-61	Qilinchang	Calcite	8.0	−57.0
14-2-8	Qilinchang	Calcite	−2.1	−66.0
Hui-8	Kuangshanchang	Barite	7.8	−86.0

Z0807-1r	15^# stope of tunnel 1752 m in Kuangshanchang	1st stage sphalerite	28.0	−52.0	d
Z0807-4r	15^# stope of tunnel 1752 m in Kuangshanchang	3rd stage sphalerite	5.5	−50.0
Z0807-5r	15^# stope of tunnel 1752 m in Kuangshanchang	3rd stage sphalerite	2.2	−55.0
Z0807-6r	15^# stope of tunnel 1752 m in Kuangshanchang	1st stage sphalerite	25.5	−50.0
Z0807-10r	15^# stope of tunnel 1752 m in Kuangshanchang	2nd stage sphalerite	17.1	−27.0
Z0807-11r	15^# stope of tunnel 1752 m in Kuangshanchang	3rd stage sphalerite	4.0	−43.0
Z0807-12r	15^# stope of tunnel 1752 m in Kuangshanchang	2nd stage sphalerite	13.2	−49.0
Z0807-13r	15^# stope of tunnel 1752 m in Kuangshanchang	2nd stage sphalerite	12.2	−57.0
Z0807-17r	15^# stope of tunnel 1752 m in Kuangshanchang	1st stage sphalerite	28.9	−51.0

JS-11-1	Qilinchang	Barite	−91.3	11.6	e
JS-11-2	Qilinchang	Barite	−85.5	9.9
JS-11-3	Qilinchang	Barite	−87.8	11.8
JS-12-1	Qilinchang	Barite	−77.4	11.8
JS-12-3	Qilinchang	Barite	−80.5	11.7
JS-13-1	Qilinchang	Barite	−79.8	12.4
JS-40-3	Kuangshangchang	Barite	−73.7	12.4
JS-40-5	Kuangshangchang	Barite	−63.9	13.7
JS-41-1	Kuangshangchang	Barite	−75.1	13.4
JS-42-2	Kuangshangchang	Barite	−61.7	13.4

a, b, c, d, and e: data from Li et al. [10], Han et al. [16], Liu and Lin [21], this paper, and Wang [47]. Different stages of sphalerite from the same ores can be separated based on textural and structural observations (Figures 3, 4, 6, and 8).