2011
DOI: 10.5382/segnews.2011-84.fea
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Paradigmatic Shifts in the Uranium Exploration Process: Knowledge Brokers and the Athabasca Basin Learning Curve

Abstract: Uranium exploration increased over the past decade in response to an increase in the price of uranium, with more than 900 companies engaged in the global exploration on over 3,000 projects. Major economic discoveries of new uranium orebodies have been elusive despite global exploration expenditures of $3.2 billion USD, with most of the effort in historical uranium districts. The increased effort in exploration with minimal return can be described through the example of a cyclical model based on exploration and… Show more

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Cited by 5 publications
(2 citation statements)
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“…The presence and disruption of graphite-bearing conductors is one of the main exploration criteria for URU deposits in the Athabasca Basin, reflecting the presence of graphite-rich fault zones within metasedimentary rocks (Hoeve & Sibbald, 1978;Jefferson et al, 2007;Kerr, 2010;Marlatt & Kyser, 2011;Potter & Wright, 2015).…”
Section: Discussion and Implications To The Ore System Modelmentioning
confidence: 99%
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“…The presence and disruption of graphite-bearing conductors is one of the main exploration criteria for URU deposits in the Athabasca Basin, reflecting the presence of graphite-rich fault zones within metasedimentary rocks (Hoeve & Sibbald, 1978;Jefferson et al, 2007;Kerr, 2010;Marlatt & Kyser, 2011;Potter & Wright, 2015).…”
Section: Discussion and Implications To The Ore System Modelmentioning
confidence: 99%
“…The presence and disruption of graphite‐bearing conductors is one of the main exploration criteria for URU deposits in the Athabasca Basin, reflecting the presence of graphite‐rich fault zones within metasedimentary rocks (Hoeve & Sibbald, 1978; Jefferson et al., 2007; Kerr, 2010; Marlatt & Kyser, 2011; Potter & Wright, 2015). In addition to facilitating fault reactivation (Kyser et al., 1989; Song et al., 2022; Yeo & Potter, 2010), graphite within the metasedimentary rocks is a potential reductant to precipitate uranium from the oxidized basin brines (e.g., Alexandre et al., 2005; Dargent et al., 2015; Hoeve & Quirt, 1984; Hoeve & Sibbald, 1978; Kyser et al., 1989; Landais et al., 1993; Pascal, Ansdell, et al., 2016; Pascal, Boiron, et al., 2016; Potter & Wright, 2015; Martz et al., 2017, 2019; Yeo & Potter, 2010).…”
Section: Discussion and Implications To The Ore System Modelmentioning
confidence: 99%