“…Some ores will be richer in certain trace elements than others. For instance, some post-Jurassic phosphates proved to have progressively heavier REE enrichments (Jiang et al, 2007), and PR ores in Quebrada del Hierro -Khalek et al, 2011;AblowSlama et al, 2014;Bunuş et al, 1994;Crouse and Brown, 1958;Ragheb and Khasawneh, 2010;Ulrich et al, 2014;c Bunuş et al, 1994;Krea and Khalaf, 2000;Lokshin et al, 2011;Pereira and Bilal, 2012;Preston et al, 1996;Wang et al, 2010Wang et al, , 2011d Van Kauwenbergh, 2006;Sadegh Safarzadeh et al, 2007;Syers, 2001;Van Kauwenbergh, 2002, 2006e Crouse and Brown, 1958;Weterings and Janssen, 1985;f Huang et al, 2010;Liu et al, 2008;Van Kauwenbergh, 2006;g Lu, 2010;Yang and Luo, 2013 , 2002). Though the average U content in PR is 0e390 ppm with a median of 61.8 ppm (Table 5), some Canadian commercial-rich ores have up to 15% (Ragheb and Khasawneh, 2010).…”