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  • Maden Tetkik ve Arama Dergisi
  • Volume:174 Issue:174
  • Economic heavy minerals in the stream sediments of wadi Shaàb, southern coast of the Red Sea, Egypt;...

Economic heavy minerals in the stream sediments of wadi Shaàb, southern coast of the Red Sea, Egypt; characterization and upgrading for investigation of their potential recovery

Authors : Mona Fawzy, Mustafa Bayoumi, Hassan Shahin, Bahaa Emad, Abdel Hay El Shafey, Marwa Abdelazeem, Ahmed Ismail, Asmaa Elmoghazy, Mohamed Diab
Pages : 145-165
Doi:10.19111/bulletinofmre.1472786
View : 19 | Download : 28
Publication Date : 2024-08-13
Article Type : Research Paper
Abstract :The southern coast of the Red Sea is one of the most promising areas for the occurrence of economic minerals. Therefore, studying the characterization and evaluation of these minerals in the Wadi Shaàb Quaternary sediments and investigating their ability to concentrate and physically separate using economical and ecofriendly techniques is the main goal of this work. The results showed that the representative sample contains an average of 0.06% ilmenite, 0.08% zircon, 0.07% rutile, 0.07% leucoxene, 0.008% cassiterite, 0.004% xenotime, 0.0004% monazite, 0.022% almandine garnet, and 0.46% magnetite. The recovery of economic heavy minerals was applied using a combination of wet-gravity technique via shaking table and magnetic separation using high intensity magnetic separator. The results demonstrated the success of gravity separation in raising the grade from 7.63% to 45.03% in a yield of 13.74% out of the original sample, and also valuable metallurgical recoveries that greater than 89% for tabling multi-stages (rougher and scavenging) was obtained. Concentrated mineral fractions of magnetite, ilmenite, almandine, heavy silicates, and the non-magnetic fraction bearing zircon and rutile were obtained using a high intensity magnetic separator at different ampere range
Keywords : Heavy Minerals, Red Sea Coast, Gravity Concentration, Magnetic Separation, Potential Recovery, Material balance

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