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-Reference-Cited by-同舟云学术

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

Published:2014-06 Issue: Volume:246 Page:35-53
ISSN:0301-9268
Container-title:Precambrian Research
language:en
Short-container-title:Precambrian Research

Author:

Hollis J.A.,Carson C.J.,Glass L.M.,Kositcin N.,Scherstén A.,Worden K.E.,Armstrong R.A.,Yaxley G.M.,Kemp A.I.S.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference94 articles.

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3. Petrochemistry and U–Pb monazite geochronology of granitic pegmatite from the Ranger U deposit;Annesley,2002

4. Significance of U–Pb detrital zircon ages in quartzite from peri-Gondwanan terranes, New Brunswick and Nova Scotia, Canada;Barr;Precambrian Research,2003

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