Plesovice zircon : A new natural reference material for U-Pb and Hf isotopic microanalysis

The origin and pre-Cenozoic evolution of the Tibetan Plateau

https://www.jcsservices.in/pdf/Huan_Fontaine_Chem_Geology.pdf

Simultaneous determinations of U-Pb age, Hf isotopes and trace element compositions of zircon by excimer laser-ablation quadrupole and multiple-collector ICP-MS

http://www.igeodata.org/bitstream/20.500.11758/350/1/Reassessment%20ofcontinentalgrowthduringtheaccretionaryhistoryof.pdf

Reassessment of continental growth during the accretionary history of the Central Asian Orogenic Belt

Models for the growth of continental crust rely on knowing the balance between the generation of new crust and the reworking of old crust throughout Earth’s history. The oxygen isotopic composition of zircons, for which uranium-lead and hafnium isotopic data provide age constraints, is a key archive of crustal reworking. We identified systematic variations in hafnium and oxygen isotopes in zircons of different ages that reveal the relative proportions of reworked crust and of new crust through time. Growth of continental crust appears to have been a continuous process, albeit at variable rates. A marked decrease in the rate of crustal growth at ~3 billion years ago may be linked to the onset of subduction-driven plate tectonics.

https://science.sciencemag.org/content/sci/335/6074/1334.full.pdf

A Change in the Geodynamics of Continental Growth 3 Billion Years Ago

Comment: Hf-isotope heterogeneity in zircon 91500

http://gemoc.mq.edu.au/TerraneChronpds/358%20Veevers.pdf

U–Pb ages and source composition by Hf-isotope and trace-element analysis of detrital zircons in Permian sandstone and modern sand from southwestern Australia and a review of the paleogeographical and denudational history of the Yilgarn Craton

Pan-Gondwanaland detrital zircons from Australia analysed for Hf-isotopes and trace elements reflect an ice-covered Antarctic provenance of 700–500 Ma age, TDM of 2.0–1.0 Ga, and alkaline affinity

Reply to “Comment to short-communication ʽComment: Hf-isotope heterogeneity in zircon 91500' by W.L. Griffin, N.J. Pearson, E.A. Belousova and A. Saeed (Chemical Geology 233 (2006) 358–363)” by F. Corfu

Gamburtsev Subglacial Mountains provenance of Permian–Triassic sandstones in the Prince Charles Mountains and offshore Prydz Bay: Integrated U–Pb and TDM ages and host-rock affinity from detrital zircons

Ayesha Saeed

Papers

Comment: Hf-isotope heterogeneity in zircon 91500

U–Pb ages and source composition by Hf-isotope and trace-element analysis of detrital zircons in Permian sandstone and modern sand from southwestern Australia and a review of the paleogeographical and denudational history of the Yilgarn Craton

Pan-Gondwanaland detrital zircons from Australia analysed for Hf-isotopes and trace elements reflect an ice-covered Antarctic provenance of 700–500 Ma age, TDM of 2.0–1.0 Ga, and alkaline affinity

Reply to “Comment to short-communication ʽComment: Hf-isotope heterogeneity in zircon 91500' by W.L. Griffin, N.J. Pearson, E.A. Belousova and A. Saeed (Chemical Geology 233 (2006) 358–363)” by F. Corfu

Gamburtsev Subglacial Mountains provenance of Permian–Triassic sandstones in the Prince Charles Mountains and offshore Prydz Bay: Integrated U–Pb and TDM ages and host-rock affinity from detrital zircons