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A palaeomagnetic study of the major volcanic units of Santa Maria reveals dominantly reverse characteristic magnetizations with a mean direction of D = 179, I = −49 and α 95 = 2.1° (85 specimens from 20 sites). Sporadically occurring normal polarity remanences are interpreted as an overprinted component imposed by the island's terminal volcanic phase (the Feteiras Formation) now primarily

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A palaeomagnetic study of the major volcanic units of Santa Maria reveals dominantly reverse characteristic magnetizations with a mean direction of D = 179, I = −49 and α 95 = 2.1° (85 specimens from 20 sites). Sporadically occurring normal polarity remanences are interpreted as an overprinted component imposed by the island's terminal volcanic phase (the Feteiras Formation) now primarily

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