Chemical heterogeneity of Mt. Etna magmas in the last 15 ce:hsp>ka. Inferences on their mantle sources
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225">We focus on the primitive basaltic magmas that bypassed Etna central conduits.

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Magma heterogeneities are linked to the melting of heterogeneous Hyblean-type mantle.

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None of the pre-1970s magmas are parent of present-day basalts.

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The ongoing selective alkali-enrichment of Etna magmas is a mantle source process.

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The decoupling of Rb–K and 87Sr–Cl reveals multistage events of mantle metasomatism.

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