2008
DOI: 10.1016/j.apgeochem.2007.12.004
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The provenance of Australian uranium ore concentrates by elemental and isotopic analysis

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Cited by 111 publications
(59 citation statements)
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“…They found that UOCs from the three operational U mines could readily be distinguished on the basis of Pb isotopes, 234 U/ 238 U, and trace elements using a multivariate statistical approach. Keegan et al (2008) also observed significant variability in rare earth element (REE) ratios between the three samples. In a study focusing on UOC from several different countries, clear differences in anion ratios and concentrations were observed between UOCs from different sources (Badaut et al 2009).…”
Section: Trace Elementsmentioning
confidence: 92%
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“…They found that UOCs from the three operational U mines could readily be distinguished on the basis of Pb isotopes, 234 U/ 238 U, and trace elements using a multivariate statistical approach. Keegan et al (2008) also observed significant variability in rare earth element (REE) ratios between the three samples. In a study focusing on UOC from several different countries, clear differences in anion ratios and concentrations were observed between UOCs from different sources (Badaut et al 2009).…”
Section: Trace Elementsmentioning
confidence: 92%
“…Despite this progress, no single parameter has yet been identified that is able to discern the identity and origin of unknown UOC samples. Increasingly, combined isotopic fingerprinting approaches are used to constrain the provenance and processing history of samples, and multivariate statistical techniques are used to discriminate between different sources of UOCs (Keegan et al 2008(Keegan et al , 2012(Keegan et al , 2014Bayne et al 2009;Robel et al 2009Robel et al , 2011Sirven et al 2009;Varga et al 2010). Likewise, approaches to chronometry have evolved over time, toward an increasing emphasis on obtaining concordant results from multiple parent, daughter, and granddaughter systems.…”
Section: Discussionmentioning
confidence: 99%
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“…As published, this presumed invariant ratio and its references cannot be traced back to the International System (SI) of Units (12). More recently, the IUPAC (13) recommend a value of 137.80 from the analysis of six natural ore deposits (14), confirmed by high-precision isotope ratio analyses using the IRMM 3636 233 U-236 U double spike (15,16) whose isotopic composition is traceable to SI units. The invariance of the present-day 238 U/ 235 U ratio has been brought into question by studies that have demonstrated U isotopic fractionation in terrestrial materials (17)(18)(19)(20).…”
mentioning
confidence: 99%
“…Using such a database, which is representative of the population(s), should enable the attribution of the type and source of such material on a scientific basis, without having to worry about the terms -unique‖ or -identification‖ [12], and should produce results which have more weight when presented in court [13,14]. It has been shown that samples from the same source show significant uniformity in trace element distribution, and significant variation between different sources, leading to good discrimination between sources [15,16]. This discrimination is also successfully used to distinguish archeological artefacts, such as coins, with different origins [17].…”
mentioning
confidence: 99%