Orogenic to anorogenic signatures in Mesozoic intra-plate magmatism: Evidence from alkali-rich dykes in the Finero Phlogopite Peridotite (Ivrea-Verbano Zone, Southern Alps) | Zendy

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Orogenic to anorogenic signatures in Mesozoic intra-plate magmatism: Evidence from alkali-rich dykes in the Finero Phlogopite Peridotite (Ivrea-Verbano Zone, Southern Alps)

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