1
Return

Separation of Au and Sb mineralization in the Qukulekedong intrusion-related deposit, East Kunlun Orogen (NW China): Evidence from fluid inclusions, H-O isotopes, and quartz geochemistry

delete2024-01-01
delete4
delete
OA
AI
L
Ling Xing
W
Wenchang Li *
X
Xiaobo Zhao
M
Mei Zang
F
Fucheng Yang
Y
Yongming Guo
Y
Yujun Shi
张正峰 (Zhengfeng Zhang)
J
Jingfeng Liu
M
Mengjun Zhang
DOI:10.1016/j.oregeorev.2023.105828delete
deleteOriginal
deleteShare
deleteSave
View PDF
Abstract

Abstract

En 中文
Separation of Au and Sb mineralization from different hydrothermal stages is a common phenomenon in many Au-Sb deposits, but its cause remains enigmatic. The Qukulekedong intrusion-related Au-Sb deposit in the East Kunlun Orogen has undergone four hydrothermal stages: (1) barren quartz vein, (2) quartz vein with disseminated arsenopyrite-pyrite alteration halo, (3) stibnite-quartz +/- native gold vein, and (4) calcite-quartz vein. Stages 2 and 3 formed disseminated Au and vein-type Sb +/- Au ore, respectively. Here, internal texture and trace elements in quartz, fluid inclusions (Fls) microthermometry, and H-O isotopes were analyzed to unravel the separation mechanism of the Au and Sb +/- Au mineralization at Qukulekedong. Stage 2 quartz has euhedral growth zones with elevated Ti-Al-Li-K-Sb and varying As contents. Stage 2 FIs have medium homogenization temperature (203-307 degrees C) and salinity (12.2-17.8 wt% NaCl equiv.), and are CH4-rich. They have delta 18OH2O = 9.5-10.8 %o and delta DH2O =-93.4 to-80.8 %o. In contrast, stage 3 quartz has lower Ti-Al-Li-K and varying Sb contents. Stage 3 FIs show phase separation (coexistence of V-, L-and V-L-type FIs), and are of lower temperature (141-164 degrees C) and salinity (2.1-10.7 wt% NaCl equiv.), and CO2- and CH4-bearing. They have delta 18OH2O = 3.3-5.2 %o and delta DH2O = -95.4 to -89.6 %o. Considering that the disseminated Au ore is Sb-rich and its pyrite has fine stibnite inclusions, we suggest that the disseminated Au and vein-type Sb +/- Au mineralization shared a common Au-and Sb-rich initial magmatic fluids. The disseminated Au mineralization may have formed by fluid-rock interactions. Meanwhile, the vein-type Sb +/- Au mineralization was likely caused by the phase separation and cooling led by dilational activities and meteoric water injection.
Keywords:
separation of Au and Sb mineralization
Intrusion -related gold system
Fluid evolution
Deposition mechanism
Qukulekedong
AI Summary

AI Summary

Key information extracted from the uploaded paper, including a brief overview, abstract, background, key highlights, visual analysis, and future outlook.

Journal

ORE GEOLOGY REVIEWS cover
ORE GEOLOGY REVIEWS
IF:
3.6
Papers:
6.4K
Citations:
2.2W

Organization

C
China University of Geosciences
Scholars:
3.7W
Papers: 2.8W
Citations: 4.3W
C
Chengdu University of Technology
Scholars:
1.2W
Papers: 6.9K
Citations: 24
Cited Papers

Cited Papers

Citing Papers

Citing Papers