2016
DOI: 10.1016/j.oregeorev.2015.12.018
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Geochemistry of platinum-group elements and mineral composition in chromitites and associated rocks from the Abdasht ultramafic complex, Kerman, Southeastern Iran

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Cited by 9 publications
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“…The Pd/Ir values, an indicator of PGE fractionation, are relatively constant in all chromitites and vary from 0.04 to 0.25 (Table 1). These patterns and the low PGE abundances are typical of ophiolitic chromitites elsewhere (Figure 4b) and indicating a high degree of partial melting of the mantle source very similar to nearby mafic-ultramafic complexes of Soghan and Abdasht [6,7]. The binary plots of TiO 2 wt.% vs. Cr# show that the massive and most disseminated chromian spinels fall in the boninitic field (Figure 5a).…”
Section: Resultsmentioning
confidence: 85%
“…The Pd/Ir values, an indicator of PGE fractionation, are relatively constant in all chromitites and vary from 0.04 to 0.25 (Table 1). These patterns and the low PGE abundances are typical of ophiolitic chromitites elsewhere (Figure 4b) and indicating a high degree of partial melting of the mantle source very similar to nearby mafic-ultramafic complexes of Soghan and Abdasht [6,7]. The binary plots of TiO 2 wt.% vs. Cr# show that the massive and most disseminated chromian spinels fall in the boninitic field (Figure 5a).…”
Section: Resultsmentioning
confidence: 85%