.png){kind=icon}
.png){kind=icon}
Return
Tracing Ag–Pb–Zn Associations with Cu–Mo Mineralization: Insights from the Oyut Porphyry Deposit, Northern Mongolia
.png){kind=icon}
OA
AI
M
O
A
B
B
A
A
N
DOI：10.1016/j.gexplo.2026.108096.png)
.png){kind=icon}
.png){kind=icon}
Share.png){kind=icon}
Save
Abstract
En 中文
• Cu–Mo mineralization is mainly hosted in Stages I–IV with evolving hydrothermal fluids. • Ag occurs exclusively in solid solution within Cu–Fe sulfides during three Ag events. • Stage IV sphalerite contains exceptionally high Au (~6000 ppm) in nano-inclusions. • Ag–Sb–Co decrease and Pb–Zn increase from early to late mineralization stages. • Ag is potential by-product metal for the Oyut Cu–Mo deposit.
Keywords:
Ag deportment
Porphyry Cu–Mo deposit
Erdenetiin-Ovoo
Northern Mongolia
AI Summary
Key information extracted from the uploaded paper, including a brief overview, abstract, background, key highlights, visual analysis, and future outlook.
Journal
IF:
3.3
Papers:
3.8K
Citations:
9.5K
Organization
Cited Papers