ABSTRACT
We use a recently completed airborne magnetic and gamma-ray spectrometric survey, and new U/Pb and 40Ar/39Ar age determinations, to revise and clarify several aspects of Brook Street Terrane geology in the Takitimu Mountains. Steeply dipping and homoclinal Permian Takitimu Subgroup formations defined in the central part of the range can, with moderate confidence, be traced along strike to other parts of the range where they are more complexly folded and faulted. We report intrusion ages for three Brook Street plutonic suites: pyroxene-bearing White Hill Intrusives (306-270 Ma, U/Pb zircon), amphibole-bearing Mackinnon Peak Intrusives (261 ± 1 Ma, 40Ar/39Ar amphibole), and shoshonitic Wether Hill Dikes (254 ± 1 Ma, 40Ar/39Ar plagioclase). Geological relationships between these intrusions and the host Takitimu Subgroup reinforce the Early Permian age of the latter, which is distinct from the overlying Late Permian Productus Creek Group. The Wether Hill Dikes mark the cessation of igneous activity in the Brook Street Terrane at c. 254 Ma. A large (n = 499) dataset of detrital zircon U/Pb ages from the nonmarine Jurassic Barretts Formation confirms a local Median Batholith-Tuhua Intrusives provenance and supports a post-Permian fore-arc tectonic setting along the Gondwana margin.
Acknowledgements
We thank Anneka Greve, Will Oliver, and High Country Helicopters of Orawia for assistance in the field, and Struan Minty of Beaumont Station and Ceri Lewis of Mount Linton Station for access. Karine Haroumi Moromizato is acknowledged for technical support and guidance. Various aspects of this work were discussed with Oliver Nebel, Richard Kellett and Donna Eberhart-Phillips. The manuscript was improved by comments from Rose Turnbull, Andy Tulloch and Carl Spandler.
Disclosure statement
No potential conflict of interest was reported by the author(s).
Data availability statement
Supplemental Files 1–5 are available in the Figshare online repository at https://doi.org/10.6084/m9.figshare.20004392. Supplemental File 1 contains whole rock geochemical methods and analytical data. Supplemental File 2 describes U/Pb isotopic methods, and contains cathodoluminescence images and age distribution plots of zircons from sample 010-TK. Supplemental File 3 is a table of all U-Pb zircon analytical data. Supplemental File 4 is a catalogue of photomicrographs of samples dated by 40Ar/39Ar methods. Supplemental File 5 describes 40Ar/39Ar methods, and contains age plots and provisional interpretive comments for all aliquots dated by 40Ar/39Ar methods.