scholarly journals THE U-Pb AGE AND Lu-Hf ISOTOPE COMPOSITION OF DETRITAL ZIRCON FROM METASEDIMENTARY ROCKS OF THE ONOT GREENSTONE BELT (Sharyzhalgay uplift, southern Siberian craton)

2014 ◽  
Vol 55 (11) ◽  
Keyword(s):  
Siberian Craton ◽  
Detrital Zircon ◽  
Greenstone Belt ◽  
Isotope Composition ◽  
Hf Isotope ◽  
Metasedimentary Rocks

scholarly journals Detrital zircon petrochronology of central Australia, and implications for the secular record of zircon trace element composition

Geosphere ◽  
2021 ◽  
Author(s):  
Charles Verdel ◽  
Matthew J. Campbell ◽  
Charlotte M. Allen
Keyword(s):  
Trace Element ◽  
Continental Crust ◽  
Detrital Zircon ◽  
Isotope Composition ◽  
Regional Scale ◽  
Large Data ◽  
Hf Isotope ◽  
Geological Time ◽  
Related Factors ◽  
Data Set

Hafnium (Hf) isotope composition of zircon has been integrated with U-Pb age to form a long-term (>4 b.y.) record of the evolution of the crust. In contrast, trace element compositions of zircon are most commonly utilized in local- or regional-scale petrological studies, and the most noteworthy applications of trace element studies of detrital zircon have been in “fingerprinting” potential source lithologies. The extent to which zircon trace element compositions varied globally over geological time scales (as, for example, zircon U-Pb age abundance, O isotope composition, and Hf isotope composition seem to have varied) has been little explored, and it is a topic that is well suited to the large data sets produced by detrital zircon studies. In this study we present new detrital zircon U-Pb ages and trace element compositions from a continent-scale basin system in Australia (the Centralian Superbasin) that bear directly on the Proterozoic history of Australia and which may be applicable to broader interpretations of plate-tectonic processes in other regions. U-Pb ages of detrital zircon in the Centralian Superbasin are dominated by populations of ca. 1800, 1600, 1200, and 600 Ma, and secular variations of zircon Hf isotope ratios are correlated with some trace element parameters between these major age populations. In particular, elevated εHf(i) (i.e., radiogenic “juvenile” Hf isotope composition) of detrital zircon in the Centralian Superbasin tends to correspond with relatively high values of Yb/U, Ce anomaly, and Lu/Nd (i.e., depletion of light rare earth elements). These correlations seem to be fundamentally governed by three related factors: elemental compatibility in the continental crust versus mantle, the thickness of continental crust, and the contributions of sediment to magmas. Similar trace element versus εHf(i) patterns among a global zircon data set suggest broad applicability. One particularly intriguing aspect of the global zircon data set is a late Neoproterozoic to Cambrian period during which both zircon εHf(i) and Yb/U reached minima, marking an era of anomalous zircon geochemistry that was related to significant contributions from old continental crust.

Detrital zircon U–Pb ages and Hf-isotope systematics from the Gadag Greenstone Belt: Archean crustal growth in the western Dharwar Craton, India

2012 ◽  
Vol 22 (3-4) ◽  
pp. 843-854 ◽  
Author(s):  
D. Srinivasa Sarma ◽  
N.J. McNaughton ◽  
Elena Belusova ◽  
M. Ram Mohan ◽  
I.R. Fletcher
Keyword(s):  
Detrital Zircon ◽  
Greenstone Belt ◽  
Dharwar Craton ◽  
Hf Isotope ◽  
Crustal Growth ◽  
Isotope Systematics
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