| Summary: | This item is only available electronically. The Rakaia Terrane comprises the majority of the basement of New Zealand, yet, to date, there are competing hypotheses as to its provenance along the Gondwana margin. These range from being adjacent to areas of Antarctica to originating against northern Queensland. To help solve these competing hypotheses, I combined the analysis of detrital zircon U-Pb geochronology with Hf isotope studies and trace element concentrations to constrain the provenance. Detrital muscovites were also dated using the 40Ar-39Ar total fusion technique. Detrital zircons yielded age populations at 1100-980 Ma, 580-450 Ma, ca. 320 Ma and ca. 230 Ma. εHf(t) values of these zircons largely range from -6 to +6 and the trace element concentrations suggest that the zircons are primarily sourced from granitoids. The 40Ar-39Ar ages yield two ages with the first at ca. 340 Ma and the second at ca. 250-220 Ma. The U-Pb ages and εHf(t) values for the Ordovician and older zircons are most similar to those from the Lachlan Fold Belt while the younger zircons show a close similarity to those from the New England Fold Belt. From multidimensional scaling maps there is a strong association between zircons from the Rakaia Terrane, north eastern Queensland and the Lachlan Fold Belt. The detrital muscovite data, however, is consistent with an exclusive New England source. Combining the data from different isotopic systems and different minerals, I interpret the provenance of the Rakaia Terrane as being derived from the New England, in the Triassic. The presence of Cambrian and Precambrian zircons, but only Phanerozoic muscovites, is interpreted as demonstrating that zircons were recycled in the New England region from older rocks now exposed in the Lachlan Orogen. These data constrain the provenance of the Rakaia Terrane and allows for more detailed reconstructions of the proto-Pacific margin of Gondwana. Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2013
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