نتایج جستجو برای: sulfide ores

تعداد نتایج: 19950  

2003

of isotopically labelled vitamin D metabolites by HPLC. Journal of Chromatography 303: 229}233. Kaspersen FM, van Acquoy J, van de Laar GLM, Wagenaars GN and Funke CW (1984) Deuterium isotope effects in mianserin. Recueil Travaux Chimique de Pay-Bas 103: 32}36. Klein PD (1966) Occurence and signiRcance of isotope fractionation during analytical separation of large molecules. Advances in Chromat...

2012
Luciano Nieddu Giuseppe Manfredi

In this paper a Pattern Recognition algorithm based on a constrained version of the k-means clustering algorithm will be presented. The proposed algorithm is a non parametric supervised statistical pattern recognition algorithm, i.e. it works under very mild assumptions on the dataset. The performance of the algorithm will be tested, togheter with a feature extraction technique that captures th...

2014
Thomas J. Matthews Manuel J. Steinbauer Elli Tzirkalli Kostas A. Triantis Robert J. Whittaker

Conservation Biogeography and Macroecology Programme, School of Geography and the Environment, University of Oxford, Oxford OX1 3QY, UK, Departamento de Cîencias Agr arias – CITAA, Azorean Biodiversity Group, Universidade dos Ac ores, Angra do Hero ısmo, Pico da Urze, 9700-042 Terceira, Ac ores, Portugal, Department of Biogeography, BayCEER, University of Bayreuth, Bayreuth D-95447, Germany, De...

Journal: :Minerals Engineering 2021

• Au and Ag deportment in an intermediate sulfidation Ag-Pb-Zn system. Deportment calculation using quantitative mineralogy, bulk mineral chemistry. Deportments are highly variable between samples due to mineralogical contrast. Gold the Freiberg district is primarily hosted by arsenopyrite electrum. Silver sulfosalts fahlore. data essential for planning of mining minerals processing operations....

Bonyadi, , Forouzesh, ,

Angouran zinc and lead deposit is located about 135 km west of Zanjan city, in the northwest of the Sanandaj-Sirjan structural zone The results of this study indicate that the dolomitic alteration occurred in the carbonate hanging-wall and the presence of ankerite in the schist footwall. The main host of ore deposit is metamorphic carbonate. The Angouran dolomite is secondary and hydrothermal. ...

Abedini, Ali, Calagari, AliAsghar, Ghasemi, mahmoud,

The Zaraj-Sou bauxite deposit (southwest of Ramsar, Mazandaran Province, northern Iran) was developed as discontinuous stratified layers and/or lenses along the boundary between carbonate rocks of the Elika (Triassic) and shales and sandstones of the Shemshak (Lower Jurassic) formations. Diaspore, kaolinite, hematite, and anatase are the major mineral phases of the ores. Texturally, the bauxite...

حبیبی مهر, مسعود, عابدینی, علی,

The Gazanjeh bauxite deposit (SE Mahabad, West-Azarbaidjan province) is a typical residual sedimentary deposit with dolomitic limestone host rock of Permian age in northwestern Iran. Calculations of normative values of minerals using obtained results from XRD and XRF analyses in a selected profile indicate that diaspore, hematite, and pyrophyllite were major mineralogical phases of this deposit...

2000
YURI AMELIN CHUSI LI A. J. NALDRETT

Assimilation of crustal rocks by mafic magmas is considered important for the formation of sulfide ores. Radiogenic isotope systems may allow one to quantify the amount of contamination and to distinguish between possible contaminants. We have studied Sm-Nd, Rb-Sr, and U-Pb isotope systems in two mafic intrusions of the Nain Plutonic Suite: the 1333 Ma Voisey’s Bay intrusion that hosts the majo...

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