Fluid Inclusion and Oxygen Isotope Constraints on the Origin and Hydrothermal Evolution of the Haisugou Porphyry Mo Deposit in the Northern Xilamulun District, NE China
Table 3
Summary of oxygen isotope data of igneous and hydrothermal minerals in Haisugou.
Sample number
Measured mineral
Measured δ18 ()
Crystallization temperature (°C)
Calculated δ18 ()
Magmatic stage
HSG43
Hornblende in fresh granite
6.4
730
8.4
HSG03
Magmatic quartz in fresh granite
8.8
730
7.9
P-stage
HSG09-32
Vein quartz with no obvious sulfide
7.7
415
4.0
HSG09-08a
Barren quartz-K-feldspar vein
9.2
457
6.3
HSG09-04
Barren quartz-K-feldspar vein
7.5
416
3.8
HSG09-15
Weakly mineralized quartz vein with K-feldspar halo
7.9
453
4.9
HSG09-44
Quartz-molybdenite vein with K-feldspar halo
7.3
430
3.9
S-stage
HSG09-09a
Quartz-molybdenite hydrothermal breccias cemented by barren quartz
6.3
306
−0.4
HSG09-21
Coarse quartz-molybdenite-sericite vein
7.0
370
2.2
HSG09-25a
Quartz-molybdenite hydrothermal breccias cemented by barren quartz
3.7
335
−2.0
HSG09-34
Quartz-molybdenite-sericite vein
6.9
289
−0.4
HSG09-28
Quartz-molybdenite-sericite-chlorite vein
6.6
323
0.5
HSG09-27
Quartz-molybdenite-chalcopyrite vein with sericite halo
6.7
323
0.6
HSG09-08b
Quartz-molybdenite vein with sericite halo, cutting early quartz-K-feldspar vein
Note. The crystallization temperatures of hydrothermal quartz samples are represented by the average homogenization temperatures of the fluid inclusion assemblages they host.