2011
DOI: 10.1016/j.apgeochem.2011.01.030
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Hydrochemistry, mineralogy and chemical fractionation of mine and processing wastes associated with porphyry copper mines: A case study from the Sarcheshmeh mine, SE Iran

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Cited by 46 publications
(28 citation statements)
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“…Fresh tailings are the primary source of trace elements. Sarcheshmeh tailings are mainly composed of quartz (42 %), albite (9 %), sericite (24 %), chlorite (11 %), orthoclase (8.3 %), and pyrite (7.5 %) (Khorasanipour et al 2011). Generally, most of trace elements in sulfidic mine wastes tailings are associated with the sulfide minerals, especially pyrite.…”
Section: Fresh Tailingsmentioning
confidence: 99%
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“…Fresh tailings are the primary source of trace elements. Sarcheshmeh tailings are mainly composed of quartz (42 %), albite (9 %), sericite (24 %), chlorite (11 %), orthoclase (8.3 %), and pyrite (7.5 %) (Khorasanipour et al 2011). Generally, most of trace elements in sulfidic mine wastes tailings are associated with the sulfide minerals, especially pyrite.…”
Section: Fresh Tailingsmentioning
confidence: 99%
“…The production of mine tailings in the Sarcheshmeh concentration plants is nearly 1,215,000 t per year (Khorasanipour et al 2011). The mean content of pyrite as a main sulfide mineral is about 7.5 % in the Sarchshmeh mine tailings (Khorasanipour et al 2011).…”
Section: Fig 1 a Central Iranian Tectono-volcanic Copper Belt And Thmentioning
confidence: 99%
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