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Relating sulfide mineral zonation and trace element chemistry to subsurface processes in the Reykjanes geothermal system, Iceland
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文摘

Sulfide mineral zonation and trace element enrichment correlate with measured isotherms.

Sulfide mineral zonation resembles that observed in high-T black smoker chimneys.

Igneous sulfides likely account for < 5% of total ore metal budget in the system.

Sulfide minerals reveal subsurface parameters relevant to the characterization of geothermal resources.

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