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Enriched lithospheric mantle keel below the Scottish margin of the North Atlantic Craton: Evidence from the Palaeoproterozoic Scourie Dyke Swarm and mantle xenoliths

Research output: Contribution to a Journal (Peer & Non Peer) › Article › peer-review

54 Citations (Scopus)
Original languageUndefined/Unknown
JournalPrecambrian Research
DOIs
Publication statusPublished - 2014

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