Unraveling rare earth element signatures in hydrothermal carbonate minerals using a source-sink system
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文摘

Trace REEY in carbonate minerals are proven markers for hydrothermal processes.

A source–sink system is adopted to conceptualize hydrothermal REEY mass transfer.

The main REEY fractionating processes are summarized in flow charts.

Examples illustrate REEY pattern ‘back-tracking’ along the fluid pathways.

Rayleigh fractionation of carbonate minerals could strongly influence REEY.

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