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Tellurium-rich mineralization in submarine magmatic–hydrothermal systems: Insights from the TA25 East vent field, Tonga arc
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DOI：10.1016/j.oregeorev.2026.107387.png)
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Abstract
En 中文
• TA25 EVF chimneys exhibit significant Te enrichment, reaching up to 1650 ppm. • Te occurs both as lattice-bound components in sulfides and discrete polymetallic tellurides and native Te. • Reduced hydrothermal fluids is a key control on lattice-bound Te incorporation into sulfides. • Fluid–seawater mixing and sulfide recrystallization promote telluride and native Te formation. • Transient polymetallic melts may also contribute to Au enrichment.
Keywords:
Tonga Arc
TA25 East vent field
Tellurium
Tellurides
Magmatic contribution
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