ABSTRACT
The peraluminous Foulwind and Windy Point Granites are important components of the Foulwind Suite – a diverse group of high field strength element-enriched Carboniferous granitoids in New Zealand’s Western Province. Four phases are identified in the Foulwind Granite (Seal Point, Siberia Bay, Tauranga Bay, Lighthouse). A new age of 324.0 ± 4.1 Ma has been obtained for the relatively undeformed Siberia Bay phase. The rocks are generally enriched in high-field strength elements and the Tauranga Bay and Lighthouse phases can be classified as ferroan A-type granites, whereas classification of the other phases is ambiguous. Sr isotope compositions were disturbed by the formation of the Paparoa Metamorphic Core Complex. Nd isotopes vary considerably and indicate involvement of multiple sources. The Nd isotope and A-type signatures can be explained by melting of mid-Paleozoic I-type granites with variable involvement of Greenland Group metasediments. The tectonic setting of the Foulwind Suite is unclear, but may be related to processes subsequent to the generation of voluminous mid-Paleozoic granitoids and amalgamation of the Buller and Takaka Terranes.
Acknowledgements
We are grateful to David Shelley and John Bradshaw who highlighted the many intriguing details of Cape Foulwind geology to us during various field excursions last century. Matt Sagar, James Scott, and an anonymous reviewer are thanked for their constructive comments, which helped improve and sharpen the manuscript, and Matt Sagar is also thanked for providing the image used in .
Disclosure statement
No potential conflict of interest was reported by the author(s).
Data availability statement
The geochemical data that support the findings of this study are openly available in figshare at https://figshare.com/s/eacf895e083bf04f6333