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

2014

Fields of Research

  • Isotope Geochemistry
  • Geochemistry Not Elsewhere Classified

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