Paleoproterozoic mantle enrichment beneath the Fennoscandian Shield: Isotopic insight from carbonatites and lamprophyres
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文摘

The isotopic geochemistry of Svecofennian carbonatites and lamprophyres is presented.

A two-stage model for mantle metasomatism in the Svecofennian Domain is supported.

The Svecofennian subcontinental lithospheric mantle bears EMII characteristics.

Recycling of organic carbon resulted in highly negative 未13C in mantle carbonates.

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