.png){kind=icon}
.png){kind=icon}
Return
Garnet microtextures and geochemistry of the Tonglushan Cu–Fe–Au skarn deposit (Edong district): Constraints on fluid evolution and skarn mineralization
.png){kind=icon}
PRE
AI
M
X
Z
S
W
Y
J
X
J
J
DOI：10.1016/j.gexplo.2026.108094.png)
.png){kind=icon}
Original request for help.png){kind=icon}
Share.png){kind=icon}
Save
Abstract
En 中文
• Phlogopite RbSr dating constrains magnetite-related skarn mineralization at ~137 Ma. • Garnet chemistry records a shift from early restricted to late more open, high-flux skarn conditions. • Strong positive Eu anomalies and LREE enrichment indicate increasingly oxidized, Cl−-rich and more acidic ore-forming fluids. • Garnet compositional vectors provide indicators for Cu–Fe–Au skarn exploration.
Keywords:
Garnet
Skarn mineralization
Fluid evolution
RbSr dating
Ore-forming fluids
Journal
IF:
3.3
Papers:
3.8K
Citations:
9.5K
Organization
Cited Papers