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The titanomagnetite oxidation state, separate ilmenite abundance and other petrological properties have been measured in specimens from 168 Miocene to Pliocene Canary Island lava flows. No correlation is found between opaque petrological parameters and natural remanence polarity regardless of the way in which the data for the lava collection is subdivided.
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Ade‐Hall et al. (1970) studied this question.
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