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

Publikation: Bidrag til tidsskriftTidsskriftartikelfagfællebedømt

  • Quinten van der Meer
  • Waight, Tod
  • AJ Tulloch
  • Martin Whitehouse
  • T. Andersen
OriginalsprogEngelsk
TidsskriftJournal of Petrology
Vol/bind56
Udgave nummer5
Sider (fra-til)849-880
Antal sider32
ISSN0022-3530
DOI
StatusUdgivet - 2018

ID: 195904304