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Altered basalt, dolerite, and gabbro samples were dredged from a previously unsampled portion of the Macquarie Ridge (47°-48° S) using the commercial fishing vessel Amaltal Explorer. The rocks show petrographic and geochemical similarity to MORB-like suites found further south along the ridge. Sedimentary rocks from the same area indicate mixed oceanic and continental New Zealand sources, with no evidence of subduction-related magmatism.
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