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10.1016/j.gexplo.2020.106664

http://scihub22266oqcxt.onion/10.1016/j.gexplo.2020.106664
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33041466!7536136!33041466
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suck abstract from ncbi


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pmid33041466      J+Geochem+Explor 2021 ; 220 (ä): 106664
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  • Mechanisms for Pd-Au enrichment in porphyry-epithermal ores of the Elatsite deposit, Bulgaria #MMPMID33041466
  • Gonzalez-Jimenez JM; Pina R; Kerestedjian TN; Gervilla F; Borrajo I; Pablo JF; Proenza JA; Tornos F; Roque J; Nieto F
  • J Geochem Explor 2021[Jan]; 220 (ä): 106664 PMID33041466show ga
  • Porphyry Cu can contain significant concentrations of platinum-group elements (PGE: Os, Ir, Ru, Rh, Pt, Pd). In this study, we provide a comprehensive in situ analysis of noble metals (PGE, Au, Ag) for (Cu-Fe)-rich sulfides from the Elatsite, one of the world's PGE-richest porphyry Cu deposits. These data, acquired using laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS), indicate that Pd was concentrated in all the (Cu-Fe)-rich sulfides at ppm-levels, with higher values in pyrite (~6?ppm) formed at the latest epithermal stage (i.e., quartz-galena-sphalerite assemblage) than in bornite and chalcopyrite (<5?ppm) from the hypogene quartz-magnetite-bornite-chalcopyrite ores. Likewise, Au is significantly more concentrated in pyrite (~5?ppm) than in the (Cu-Fe)-rich sulfides (
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