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 - Result

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

Research output: Contribution to journal › Journal article › Research › peer-review

Quinten van der Meer
Waight, Tod
AJ Tulloch
Martin Whitehouse
T. Andersen

Original language	English
Journal	Journal of Petrology
Volume	56
Issue number	5
Pages (from-to)	849-880
Number of pages	32
ISSN	0022-3530
DOIs	https://doi.org/10.1093/petrology/egy047
Publication status	Published - 2018

ID: 195904304