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Trace element systematics of pyrite from submarine hydrothermal vents
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Global data base of trace element pyrite chemistry.

Most trace elements in hydrothermal pyrite are independent of the magmatic host rock composition.

Fluid–sediment interaction and serpentinization processes affect the composition of hydrothermal pyrite.

Fluid temperature variations control the trace element composition of pyrite.

Phase separation and magmatic volatiles also influence the pyrite composition.

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