Lavas and dikes in Rarotonga were sampled at 12 sites and are all found to be of reversed polarity. The mean directions of remanence are found to be 223°, + 59°, for samples from the Avatiu Valley and 180°, + 48°, for samples from the Tuoro quarry; the average circular standard deviations are 47° and 20° respectively. Insufficient sampling prevents interpretation in terms of secular variation.
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D. H. Tarling (1967) studied this question.
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