Provenance analysis of the Late Cretaceous to Paleocene Rakopi, North Cape, and Farewell formations, northwest Nelson, New Zealand
The Taranaki Basin of New Zealand first developed in the middle of the Cretaceous as Zealandia rifted from Gondwana. Rift basins were active depocentres throughout the Late Cretaceous to Paleocene when rifting slowed. The only outcrops are located in northwest Nelson in the Pakawau sub-basin, a nort...
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| Format: | Article in Journal/Newspaper |
| Language: | English |
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University of Canterbury
2018
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| Online Access: | https://dx.doi.org/10.26021/8970 https://ir.canterbury.ac.nz/handle/10092/15581 |