Paleozoic metasomatism at the origin of Mediterranean ultrapotassic magmas: Constraints from time-dependent geochemistry of Colli Albani volcanic products (Central Italy)
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文摘

Phlogopite-bearing mantle characterized by local isotopic disequilibrium

Disequilibrium melting process operating at the local scale in the metasomatized mantle

Timing of the mantle metasomatism at the origin of the ultrapotassic quaternary magmatism in the Mediterranean area

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