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Altered basalt, dolerite, and gabbro were collected from a previously unsampled portion of the Macquarie Ridge (47°-48° S). These rocks, dredged using the commercial fishing vessel Amaltal Explorer, show petrographic and geochemical similarity to MORB-like suites found further south along the ridge. The data suggests the northern ridge is geologically related to the rest of the ridge, despite its bathymetric connection to the New Zealand continental shelf.
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