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İZMİR-ÖDEMİŞ YÖRESİNDEKİ ARSENOPİRİTLERLE İLİŞKİLİ ALTIN OLUŞUMLARININ MADEN JEOLOJİSİ

open access: yesBulletin of the Mineral Research and Exploration, 2008
Bu çalışma İzmir-Ödemiş bölgesinin kuzeydogusunda yer alan Elmacıgedigi, Zeytinlik, Yılanlıkale ve Kemer yörelerinde yüzeyleyen damar görünümlü altın içeren arsenopirit oluşumlarının ve onların yakın civarlarında izlenen mikaşist, amfibol şist ve ...
Sinan AKISKA   +2 more
doaj  

Stability and solubility of arsenopyrite, FeAsS, in crustal fluids.

open access: yes, 2002
The stability and solubility of natural arsenopyrite (FeAsS) in pure water and moderately acid to slightly basic aqueous solutions buffered or not with H2 and/or H2S were studied at temperatures from 300 to 450°C and pressures from 100 to 1000 bar.
Kara, Sami   +2 more
core   +3 more sources

Approaches to Improve the Bioleaching of Arsenopyrite Flotation Concentrate with Acidithiobacillus ferrooxidans: A Comparison of Two Strains of Different Origin

open access: yesEngineering Proceedings
Bacterial leaching is a well-known green technology proposed for the extraction of valuable metals into solution. However, this biotechnology has some “bottle neck” problems too.
Tatiana Abashina   +3 more
doaj   +1 more source

The Effects of Surface Disturbances on the Leaching of Heavy Metals [PDF]

open access: yes, 1987
The harmful effects of heavy metal contamination of surface waters impacted by gold mining activity are well documented. An examination was conducted on the effects of surface disturbances in Wade Creek on the concentrations of heavy metals in ...
Brown, Edward J., Dixson, David P.
core  

Bismuth tellurides and sulphosalts from the Larga hydrothermal system, Metaliferi Mts., Romania: Paragenesis and genetic significance [PDF]

open access: yes, 2004
© 2004 Mineralogical Society of Great Britain and IrelandIntermediate levels of the Larga-Fata Baii field, Metaliferi Mts., Romania, are host to epithermal vein mineralization, small skarn-like bodies and ‘geode’-like replacement ores, that together form
Alderton   +38 more
core   +1 more source

Studies on Nickel and Cobalt in Arsenopyrites. I. Estimation and Determination of Cobalt in Some Arsenopyrites [PDF]

open access: yesBulletin of the Chemical Society of Japan, 1943
Abstract Nitroso-R-salt method has been investigated for the purpose of determining a minute quantity of cobalt in minerals. In some previous papers it was reported that the method is very satisfactory for determining cobalt in plants, soils and animal nutritions.
openaire   +1 more source

Effects of Ultrasonic Power and Intensity of Mechanical Agitation on Pretreatment of a Gold-Bearing Arsenopyrite

open access: yesArchives of Acoustics
In this paper, the effects of an ultrasonic power and the intensity of mechanical agitation for pulp on alkaline pretreatment of gold-bearing arsenopyrite were investigated.
Won Chol HONG   +3 more
doaj   +1 more source

Draa Sfar, Morocco: A Visean (331 Ma) pyrrhotite-rich, polymetallic volcanogenic massive sulphide deposit in a Hercynian sediment-dominant terrane [PDF]

open access: yes, 2008
International audienceDraa Sfar is a Visean, stratabound, volcanogenic massive sulphide ore deposit hosted by a Hercynian carbonaceous, black shale-rich succession of the Jebilet terrane, Morocco. The ore deposit contains 10 Mt grading 5.3 wt.% Zn, 2 wt.%
Belkabir, Abdelhay   +4 more
core   +6 more sources

Infrared spectra of some sulfides and their analogs of binary composition in the long-wave region [PDF]

open access: yes
The far infrared spectra (500-60/cm) of some simple sulfides and their analogs were studied. In all, 22 minerals with different structure types were investigated, out of which 14 are sulfides (galena, alabandite, pyrrhotite, sphalerite, wurtzite ...
Povarennykh, A. S.   +3 more
core   +1 more source

Mineralogy of sulfides [PDF]

open access: yes, 2017
Metal sulphides are the most important group of ore minerals. As shown in this brief introduction, much is known about their compositions, crystal structures, phase relations and paragenesis.
Becker   +31 more
core   +1 more source

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