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- W2166182007 abstract "Hornblende-rich lamprophyric dykes from southeastern Nova Scotia are contemporaneous with the large peraluminous granitic batholiths (ca. 370 Ma) of the Meguma Zone and may be closely associated with their origin." @default.
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- W2166182007 date "1989-03-01" @default.
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- W2166182007 title "Late Devonian lamprophyric dykes in the Meguma Zone of Nova Scotia" @default.
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- W2166182007 doi "https://doi.org/10.1139/e89-052" @default.
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