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

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

Detrital zircon age and Hf isotope patterns for the Cahill Formation and Nourlangie Schist are distinctly different from other Paleoproterozoic successions in the North Australian Craton. The Cahill Formation and Nourlangie Schist comprise the bulk of the Paleoproterozoic strata in the Nimbuwah Doma...

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Bibliographic Details
Main Authors: Hollis, Julie, Carson, C., Glass, L., Kositcin, N., Scherstén, A., Worden, K., Armstrong, R., Yaxley, G., Kemp, A.
Format: Journal Article
Published: Elsevier BV 2014
Online Access:http://hdl.handle.net/20.500.11937/63426

Internet

http://hdl.handle.net/20.500.11937/63426

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