Forging isotopically juvenile metamorphic zircon from and within Archean TTG gneiss: Whole-rock Sr-Nd-Pb and zircon U-Pb-Hf-REE constraints

Author:

Strong J.W.D.,Cawood P.A.,Cruden A.R.,Nebel O.,Mulder J.,Dickin A.P.

Funder

Australian Research Council

Monash University

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference59 articles.

1. Early-middle Archean crustal evolution deduced from Lu-Hf and U-Pb isotopic studies of single zircon grains;Amelin;Geochim. Cosmochim. Acta,2000

2. Behavior of isotopic systematics during deformation and metamorphism: a Hf, Nd and Sr isotopic study of mylonitized granite;Barovich;Contrib. Mineral. Petrol.,1992

3. Hafnium isotopes in zircons document the gradual onset of mobile-lid tectonics;Bauer;Geochemical Perspectives Letters,2020

4. A LA-ICP-MS evaluation of Zr reservoirs in common crustal rocks: Implications for Zr and Hf geochemistry, and zircon-forming processes;Bea;Can. Mineral.,2006

5. Geological, Geochemical and Rb-Sr and U-Pb zircon geochronological investigations of granitoid rocks from the Winnipeg River Belt, Northwester Ontario and Southeastern Manitoba [Ph.D. thesis];Beakhouse,1983

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