The Kawakawa Tephra is defined to include an upper Oruanui Breccia Member , a middle Scinde Island Ash Member , and a lower Aokautere Ash Member . It is recommended that the use of the name Oruanui Formation be discontinued. A type section is proposed together with a series of reference sections for the areas peripheral to the eruptive source.
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Vucetich et al. (1976) studied this question.
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