1986
DOI: 10.2113/gsecongeo.81.5.1278
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The development of platinum-group minerals in laterites

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Cited by 138 publications
(107 citation statements)
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“…Where conditions were compatible with the stability field of palladium, native palladium would have formed from the Pd-O phase (cf. stability diagrams of Bowles 1986, Wood et al 1989, Olivo & Gammons 1996. On the other hand, the presence of some mercury in the Pd-O-bearing phase may also suggest involvement of a low-temperature hydrothermal fluid.…”
Section: Native Palladiummentioning
confidence: 99%
“…Where conditions were compatible with the stability field of palladium, native palladium would have formed from the Pd-O phase (cf. stability diagrams of Bowles 1986, Wood et al 1989, Olivo & Gammons 1996. On the other hand, the presence of some mercury in the Pd-O-bearing phase may also suggest involvement of a low-temperature hydrothermal fluid.…”
Section: Native Palladiummentioning
confidence: 99%
“…One of the questions refers to secondary growth of platinum-group minerals (PGM) in laterites (e.g., Bowles 1986Bowles , 1995. The neoformation of PGM in the supergene environment has been advocated by some authors, whereas others have concluded that the PGM in placer deposits are of magmatic origin [vide Wood (2002) for a comprehensive list of references].…”
Section: Introductionmentioning
confidence: 99%
“…This difference has created debate concerning whether supergene processes could be responsible for the observed mineralogical differences. It has been suggested [5][6][7] that some of the PGM from the host rocks were altered during weathering and the platinum-group elements (PGE) products transported in solution to a regime of changed Eh and pH where growth of a new PGM suite occurred. Others consider this to be a "scientifically untenable hypothesis" [8].…”
Section: Introductionmentioning
confidence: 99%
“…There is textural evidence in the alluvial PGM, however, that is consistent with low-temperature growth and re-solution and re-growth. Aware of the abundant organic material and microbial fauna beneath the tropical rain forest cover of the intrusion and the ease with which the PGE react with organic materials [9,10], some studies [11][12][13] have examined the possible role of humic and fulvic acid in taking the PGE into solution at 25 • C. It is clearly possible for the PGE to enter solution under these conditions within a short time frame. Importantly, recent work has shown the ability of bacteria to play a part in the growth of PGM [14,15].…”
Section: Introductionmentioning
confidence: 99%
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