Academic literature on the topic 'Sphalerite Fe Content'

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Journal articles on the topic "Sphalerite Fe Content"

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Damian, Gheorghe, Andrei Buzatu, Andrei Ionuţ Apopei, Floarea Damian, and Andreea Elena Maftei. "Hydrothermal Sphalerites from Ore Deposits of Baia Mare Area." Minerals 11, no. 12 (2021): 1323. http://dx.doi.org/10.3390/min11121323.

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Sphalerite is an abundant mineral in the hydrothermal deposits from the Baia Mare and Oaș areas (northwestern Romania). Sphalerite samples were analyzed with an electron probe microanalyzer and Raman spectroscopy. The obtained results indicated different amounts of Fe in the various deposits from the Baia Mare and Oaș areas. The sphalerites from Baia Sprie, Cavnic, Iba, Turț Penigher, and Breiner have a low Fe wt.% content. High Fe wt.% contents are at Herja and partly at Ghezuri and Nistru (copper stage) where sphalerite is associated with pyrrhotite. The correlation between iron and zinc fro
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Motloba, G. B., K. S. Viljoen, D. H. Rose, and A. J. B. Smith. "The processing behaviour of the sphalerites from the Big Syncline deposit, South Africa." South African Journal of Geology 127, no. 1 (2024): 71–94. http://dx.doi.org/10.25131/sajg.127.0018.

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Abstract Big Syncline is one of the few unexploited deposits of the Aggeneys-Gamsberg Ore District of the Northern Cape Province of South Africa and comprises Zn > Pb > Cu mineralisation. Future exploitation of this deposit requires a good understanding of the mineralisation textures and mineralogy for beneficiation purposes. Two of the most commonly occurring mineralisation types at Big Syncline, the mineralised pelitic schist (PEL) and garnet-magnetite-associated mineralisation (GM), are investigated with regards to sphalerite petrography and mineralogy and their potential impa
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Yatimov, U. A., V. V. Maslennikov, and D. A. Artem’ev. "Geochemical features of sulfides of the Aktash magnetite-polymetallic deposit, Western Karamazar, Tajikistan (LA-ICP-MS data)." МИНЕРАЛОГИЯ (MINERALOGY) 9 (September 29, 2023): 50–69. http://dx.doi.org/10.35597/2313-545x-2023-9-3-4.

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The distribution of trace elements in sulfdes from various ores of the Aktash magnetite-polymetallic deposit (Tajikistan) is studied using LA-ICP-MS method. Sulfdes partly replace banded magnetite ores. Each sulfde type exhibits specifc geochemical features. Galena from sulfde-magnetite ores contains the higher amount of elements of «high-temperature» association (Bi, Ag, Cu) than galena from pyroxene-sphalerite ores, which, in addition to Ag and Bi, also contains higher amount of elements of «medium-temperature» association (Se, Te, and Sb). Sphalerite from sulfde-magnetite and chlorite-pyrrh
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Tămaș, Călin Gabriel, Mădălina Paula Andrii, Réka Kovács, Sergiu Drăgușanu, and Béatrice Cauuet. "Sphalerite Composition in Low- and Intermediate-Sulfidation Epithermal Ore Bodies from the Roșia Montană Au-Ag Ore Deposit, Apuseni Mountains, Romania." Minerals 11, no. 6 (2021): 634. http://dx.doi.org/10.3390/min11060634.

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We evaluated the significance of the iron and manganese content in sphalerite as a tool for distinguishing between low-sulfidation and intermediate-sulfidation epithermal deposits on the basis of new and previously published electron probe microanalyses data on the Roșia Montană epithermal ore deposit and available microchemical data from the Neogene epithermal ore deposits located in the Apuseni Mountains and Baia Mare region, Romania. Two compositional trends of the Fe vs. Mn content in sphalerite were delineated, a Fe-dominant and a Mn-dominant, which are poor in Mn and Fe, respectively. Th
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Cẩn, Phạm Ngọc, Trần Tuấn Anh, Trần Trọng Hòa та ін. "ĐẶC ĐIỂM QUẶNG HÓA VÀ KHOÁNG VẬT CÁC MỎ KẼM CHÌ KHU VỰC LÀNG HÍCH". VIETNAM JOURNAL OF EARTH SCIENCES 33, № 1 (2011): 85–93. http://dx.doi.org/10.15625/0866-7187/33/1/281.

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Chemical and mineralogical characteristics of Zn-Pb ores in Lang Hich areaLang Hich ore deposit consisting of 6 mining places (West Metis, East Metis, Hang Chua, Bac Lau, Mo Ba - 1Aoven, Mo Ba - 1B) was discovered in 1905 and has been exploited since 1913. Anually, the mine have been exploited ~20000 T, inspite of lacking detail investigation in mineralogy and chemistry of ores.Two mineral assemblages have been clafsified in Lang Hich deposit as followed : 1) pyrite-galenite-sphalerite (Metis,Mo Ba), 2) galenite-sphalerite (Bac Lau, Hang Chua). Basically, sphalerites, have low Fe, In contents
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Doucet, Pierre, Wulf Mueller, and Francis Chartrand. "Alteration and ore mineral characteristics of the Archean Coniagas massive sulfide deposit, Abitibi belt, Quebec." Canadian Journal of Earth Sciences 35, no. 6 (1998): 620–36. http://dx.doi.org/10.1139/e98-009.

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The Coniagas Mine in the northeastern Abitibi greenstone belt is a small, isolated Archean, volcanic-hosted, massive sulfide deposit rich in Zn-Pb-Ag. The Main lens, which is part of four massive sulfide lenses, is restricted to a 40 m thick massive felsic lapilli tuff unit of the 280 m thick sequence. The massive sulfides, a product of subsurface replacement, have features common to both Mattabi- and Noranda-type deposits. The Coniagas Mine sequence represents part of a small subaqueous volcanic edifice that probably evolved close to an arc or back-arc spreading ridge. A distinct alteration h
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Nagase, Toshiro, and Shoji Kojima. "An SEM examination of the chalcopyrite disease texture and its genetic implications." Mineralogical Magazine 61, no. 404 (1997): 89–97. http://dx.doi.org/10.1180/minmag.1997.061.404.09.

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AbstractBack-scattered electron imaging with a scanning electron microscope was applied to the intimate association of fine chalcopyrite grains and sphalerite (‘chalcopyrite disease’) in synthesized products and natural specimens, in order to distinguish between diagnostic features of two formation mechanisms: replacement and coprecipitation. In the synthetic chalcopyrite disease in Fe-bearing sphalerite formed by a replacement reaction, chalcopyrite occurs as fine lamellae, which are also observed in relatively Fe-rich growth bands of the natural zoned sphalerite. Ellipsoidal to lens-like hab
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Pratt, Allen, Lucia Zuin, Y. Mui Yiu, and Sarah Harmer. "High-resolution XANES S L3,2 edge spectra collected from a series of iron-bearing sphalerite(Zn,Fe)S minerals." Canadian Journal of Chemistry 85, no. 10 (2007): 761–66. http://dx.doi.org/10.1139/v07-072.

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High-resolution S L3,2-edge XANES spectra have been collected from a series of high-quality sphalerite samples. Each of the sphalerite samples examined has a characteristic iron concentration, and the range is from <0.01 to 14.79 wt% Fe. The structures of the S L3,2-edges are investigated by comparing ab initio calculated spectra with experimentally measured S L3,2-edge spectra collected from synthetic ZnS sphalerite. The theoretical and experimental data provide evidence that S 2p electron transitions to empty S 3s and S 3d states can occur across an energy range above the absorption edge.
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Bryukhov, S. I., D. A. Artem’yev, I. A. Blinov, N. R. Ayupova, and A. S. Tseluyko. "Gold-sulfide mineralization of quartz veins in granites of the South Sukhtelya gold occurrence (South Urals)." МИНЕРАЛОГИЯ (MINERALOGY) 11, no. 2 (2025): 70–87. https://doi.org/10.35597/2313-545x-2025-11-2-4.

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The paper considers mineralogical and geochemical features of gold-sulfde mineralization of quartz veins in granites of the Katsbakh complex in the South Sukhtelya gold occurrence (South Urals). The sulfde content of quartz veins varies from 1 to 3 vol. %, rarely reaching 10 vol. %, and the average Au content is 5–10 g/t. Three types of native gold are identifed: 1) in assemblage with Fe oxyhydroxides and in quartz (the fneness of 649–830 ‰), 2) in assemblage with tourmaline (the fneness of 870–888 ‰) and 3) in Fe oxyhydroxides in assemblage with fschesserite and in secondary Cu minerals. The
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Lipko, Sergey, Vladimir Tauson, and Valeriy Bychinskii. "Gold Partitioning in a Model Multiphase Mineral-Hydrothermal Fluid System: Distribution Coefficients, Speciation and Segregation." Minerals 10, no. 10 (2020): 890. http://dx.doi.org/10.3390/min10100890.

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The characteristics of Au partitioning in a multiphase, multicomponent hydrothermal system at 450 °C and 1 kbar pressure were obtained using experimental and computational physicochemical modelling and laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) analysis. Sphalerite and magnetite contained 0.1–0.16 ± 0.02 µg/g Au and coexisted with galena and bornite which contained up to 73 ± 5 and 42 ± 10 µg/g Au, respectively. Bornite and chalcopyrite were the most effective Au scavengers with cocrystallization coefficients Au/Fe and Au/Cu in mineral-fluid system n–n × 10−2. Spha
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Conference papers on the topic "Sphalerite Fe Content"

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Kontak, Daniel J., Suzanne Paradis, Zach Waller, and Mostafa Fayek. "Mineralogical and chemical characterization of Mississippi Valley–type mineralization in British Columbia and Alberta, Canada: Implications for ore-forming processes." In Irish-type Zn-Pb deposits around the world. Irish Association for Economic Geology, 2023. http://dx.doi.org/10.61153/evjz9918.

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A comprehensive study of samples from MVT–type base-metal (Zn-Pb) deposits from across the Canadian Cordillera was done to compare and contrast features and assess their relevance in the context of sulphide mineralization. Petrography and supported CL imaging indicates early host rock dissolution to form secondary fine-grained dolostone during marine cementation is followed by multiple generations of dolomite cements (low T, fine-grained to coarser, higher T varieties) that overlaps with Zn-Pb sulphides which is succeeded by a later barren calcite stage. Ore-stage dolomite is often rich in Fe
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