Quantitative analysis of New Zealand-Antarctica plate motions during the Paleogene and Late Cretaceous
Quantifying past motions of tectonic plates in the southwest Pacific is important because the Pacific-Antarctic ridge is the only non-destructive boundary between the Pacific plate and other major plates. However, formation of sea-ice near Antarctica impairs the collection of magnetic anomaly data t...
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Format: | Thesis |
Language: | unknown |
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2017
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Online Access: | https://doi.org/10.26686/wgtn.17060495.v1 |