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Garnet and epidote chemistry of the Dulong Sn-Zn-In polymetallic deposit, SW China: Constraints on the hydrothermal fluid evolution and implications for exploration
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DOI：10.1016/j.gexplo.2026.108103.png)
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Abstract
En 中文
• The garnet and epidote are enriched in In and Sn. • Enrichment of In and Sn is significantly influenced by oxygen fugacity. • Garnet UPb dating links mineralization to a regional large-scale WSn metallogenic event. • Garnet and epidote chemistry can serve as effective vectors for SnIn exploration.
Keywords:
Garnet
Epidote
Tin
Indium
Hydrothermal fluid
Journal
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3.3
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3.8K
Citations:
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