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 tidsskrift › Tidsskriftartikel › fagfællebedømt
Originalsprog | Engelsk |
---|---|
Tidsskrift | Journal of Petrology |
Vol/bind | 56 |
Udgave nummer | 5 |
Sider (fra-til) | 849-880 |
Antal sider | 32 |
ISSN | 0022-3530 |
DOI | |
Status | Udgivet - 2018 |
ID: 195904304