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M.S.
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lower crust
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ThesisClements, BrianPlate reconstructions document a polyphase rifting history of the Zealandia microcontinent, from Cretaceous continental breakup, to Tertiary intraplate rifting (Lamarche et al., 1997; Gaina et al., 1998; Sutherland, 1999; Cande and Stock, 2004; Schell . . .