Mantle plumes and Antarctica-New Zealand rifting: evidence from mid-Cretaceous mafic dykes

Ocean floor magnetic anomalies show that New Zealand was the last continental fragment to separate from Antarctica during Gondwana break-up, drifting from Marie Byrd Land, West Antarctica, about 84 Ma ago. Prior to continental drift, a voluminous suite of mafic dykes (dated by Ar–Ar laser stepped he...

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Bibliographic Details
Published in:Journal of the Geological Society
Main Authors: Storey, Bryan C., Leat, Philip T., Weaver, Stephen D., Pankhurst, Robert J., Bradshaw, John D., Kelley, Simon
Format: Article in Journal/Newspaper
Language:unknown
Published: Geological Society of London 1999
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/503806/
https://doi.org/10.1144/gsjgs.156.4.0659