Magmatic Evolution during the Cretaceous Transition from Subduction to Continental Break-up of the eastern Gondwana Margin (New Zealand) documented by in-situ Zircon O-Hf Isotopes and Bulk Rock Sr-Nd Isotopes
Quinten van der Meer, Tod Earle Waight, AJ Tulloch, Martin Whitehouse, T. Andersen
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