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Introduction
The demand for the raw material quartz is increasing worldwide, in particular, the demand for 
high-purity quartz (HPQ; e.g. /1, 2/). Therefore, quartz has been recently considered as a strategic 
mineral because it represents the raw material for special applications in high-tech industry. The 
trace-element contents of quartz are its most important quality criteria. Quartz is designated high 
purity when it contains less than 50 μg g−1 of impurities /3/, which mainly comprise structurally 
bound trace elements (B, Li, Al, Ge, Ti, Fe, Mn, Ca, K, Na and P) in the quartz lattice, also micro-
inclusions of minerals and trapped fluids. HPQ is rare in nature and larger deposits even more so. 
The few HPQ deposits found around the world include certain types of quartz-rich granitic 
pegmatite /4, 5/ and hydrothermal quartz veins. Al and Ti besides Li, P and B are used as indicators 
of the quality of the quartz. These elements are important quality-determining trace elements 
depending on the industrial application being considered for the raw material. High Ti 
concentrations, for example, change the absorption behavior of optical silica glass. Metallic silicon 
and polysilicon are bred in quartz crucibles, and high P and B concentration in the quartz glass of 
the crucibles contaminates the growing silicon crystals, which are used for solar cells or computer 
chips. Moreover, Al, Ti and Li are difficult to remove during refinement of quartz. Therefore, the 
industry is highly interested in quartz resources with low initial trace-element concentrations to 
lower production costs and to improve the quality of the quartz products. But when these resources 
are not available affordable industrial dressing becomes a necessity /6/. 
Methods and Techniques 
The methods and techniques that have been applied on the quartz deposits of Wadi Mubarak 
are: 1) Geochemical analyses by using the XRF technique and 2) Beneficiation processes 
(Floatation followed by wet magnetic separation). All the geochemical analyses and upgrading 
processes were carried out in the labs of the Egyptian geological survey. 


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