2017
DOI: 10.1134/s0097807816060051
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Geochemical features of rare-earth elements in surface and subsurface waters in the field of the Albynskoe Gold-Bearing Placer, Amur oblast

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Cited by 5 publications
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“…The existence of a geochemical barrier here is evidenced not only by the appearance of numerous newly formed crystals of native gold but also by the presence of supergene cerianite-(Ce) (Figure 6d). There is also an abrupt increase in Ce* values (up to ~1.1, Figure 5), which is probably caused by oxidation of the element to the low-soluble Ce 4+ and its removal from aqueous solutions in the form of CeO2 [54][55][56][57][58][59][60].…”
Section: Discussion Of the Oxidized Ores Formation Conditionsmentioning
confidence: 99%
“…The existence of a geochemical barrier here is evidenced not only by the appearance of numerous newly formed crystals of native gold but also by the presence of supergene cerianite-(Ce) (Figure 6d). There is also an abrupt increase in Ce* values (up to ~1.1, Figure 5), which is probably caused by oxidation of the element to the low-soluble Ce 4+ and its removal from aqueous solutions in the form of CeO2 [54][55][56][57][58][59][60].…”
Section: Discussion Of the Oxidized Ores Formation Conditionsmentioning
confidence: 99%