Detrital zircon U-Pb-Hf and O isotope character of the Cahill Formation and Nourlangie Schist, Pine Creek Orogen: Implications for the tectonic correlation and evolution of the North Australian Craton
Citation
Hollis, J, Carson, C, Glass, L et al 2014, 'Detrital zircon U-Pb-Hf and O isotope character of the Cahill Formation and Nourlangie Schist, Pine Creek Orogen: Implications for the tectonic correlation and evolution of the North Australian Craton', Precambrian Research, vol. 246, pp. 35-53.Year
2014ANU Authors
Fields of Research
- Isotope Geochemistry
- Geochemistry Not Elsewhere Classified