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Chilled margin and marginal reversal formation in the Koillismaa Deep Intrusion: implications for parental magma compositions in the 2.44 Ga Tornio–Näränkävaara Belt

Crossref DOI link: https://doi.org/10.1007/s00410-025-02226-4

Published Online: 2025-07-02

Published Print: 2025-07

Update policy: https://doi.org/10.1007/springer_crossmark_policy

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