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Granite-hosted,Nb-,Ta-,Sn-,U-,Th-,and Zr(Hf)-bearing mineralization from the Abu Rusheid shear zones occurs about 97 km southwest of the town of Marsa Alam,South Eastern Desert,Egypt.The SSE-trending brittle-ductile Abu Rusheid shear zones crosscut the peralkalic granitic gneisses and cataclastic to mylonitic rocks(mylonite,protomlyonite,and ultramylonite).The northern shear zone varies in width from 1 to 3 m with a strike length of >500 m,and the southern shear zone is 0.5 to 8 m wide and >1 km long.These shear zones locally host less altered lamprophyre and locally sheared granitic aplite-pegmatite dykes.The rare-metal minerals,identified from the peralkalic granitic gneisses and cataclastic to mylonitic rocks are associated with muscovite,chlorite,quartz,fluorite,pyrite,magnetite,and rare biotite that are restricted to the Abu Rusheid shear zones;these are columbite-tantalite and pyrochlore(var.betafite) in the northern shear zone and ferrocolumbite in the southern shear zone.Cassiterite occurs as inclusions in the columbite-tantalite minerals.U-and Th-minerals(uraninite,thorite,uranothorite,ishikawaite,and cheralite) and Hf-rich zircon coexist.Magmatic(?) zircon contains numerous inclusions of rutile,fluorite,U-Th and REE minerals,such as uranothorite,cheralite,monazite,and xenotime.Compositional variations in Ta/(Ta+Nb) and Mn/(Mn+Fe) in columbite range from 0.07-0.42 and 0.04-0.33,respectively,and Hf contents in zircon from 1.92-6.46 of the two mineralized shear zones reflect the extreme degree of magmatic fractionation.Four samples of peralkalic granitic gneisses and cataclastic to mylonitic rocks from the southern shear zone have very low TiO2(0.02 wt%-0.04 wt%),Sr [(15-20)×10-6],and Ba [(47-78)×10-6],with high Fe2O3T(0.94 wt%-1.99 wt%),CaO(0.14 wt%-1.16 wt%),alkalis(9.2 wt%-10.1 wt%),Rb [(369-805)×10-6],Zr [(1033-2261)×10-6],Nb [(371-913)×10-6],U [(51-108)×10-6],Th [(36-110)×10-6],Ta [(38-108)×10-6],Pb [(39-364)×10-6],Zn [(21-424)×10-6],Y [(8-304)×10-6],Hf [(29-157)×10-6],and ∑REE [(64-304)×10-6],especially HREE [(46-167)×10-6].Three samples from the northern shear zone also have very low TiO2(0.03 wt%),Sr [(11-16)×10-6],and Ba [(38-47)×10-6],with high Fe2O3T(1.97 wt%-2.91 wt%),CaO(0.49 wt%-1.01 wt%),alkalis(7.2 wt%-8.3 wt%),Rb [(932-978)×10-6],Zr [(1707-1953)×10-6],Nb [(853-981)×10-6],Ta [(100-112)×10-6],U [(120-752)×10-6],Th [(121-164)×10-6],Pb [(260-2198)×10-6],Zn [(483-1140)×10-6],Y [(8-304)×10-6],Hf [(67-106)×10-6],and ∑REE [(110-231)×10-6],especially HREE [(91-177)×10-6].The very high Rb/Sr(57.5-88.9),and low Zr/Hf(16.9-25.6),Nb/Ta(7.7-9.8),and Th/U(0.21-1.01) are consistent with very frac-tionated fluorine-bearing granitic rocks that were altered and sheared.The field evidence,textural relations,and compositions of the ore minerals suggest that the main mineralizing event was magmatic(629+/-5 Ma,CHIME monazite),with later hydrothermal alteration and local remobilization of the high-field-strength elements.
Granite-hosted, Nb-, Ta-, Sn-, U-, Th-, and Zr (Hf) -bearing mineralization from the Abu Rusheid shear zones occur about 97 km southwest of the town of Marsa Alam, South Eastern Desert, Egypt The SSE-trending brittle-ductile Abu Rusheid shear zones crosscut the peralkalic granitic gneisses and cataclastic to mylonitic rocks (mylonite, protomlyonite, and ultramylonite). The northern shear zone varies in width from 1 to 3 m with a strike length of> 500 m, and the southern shear zone is 0.5 to 8 m wide and> 1 km long. The shear zones zones host less altered lamprophyre and locally sheared granitic aplite-pegmatite dykes. the rare-metal minerals, identified from the peralkalic granitic gneisses and cataclastic to mylonitic rocks are associated with muscovite, chlorite, quartz, fluorite, pyrite, magnetite, and rare biotite that are restricted to the Abu Rusheid shear zones; these are columbite-tantalite and pyrochlore (var.betafite) in the northern shear zone and ferrocolumbite in the southern shear zone. Cassit erite occurs as inclusions in the columbite-tantalite minerals.U-and Th-minerals (uraninite, thorite, uranothorite, ishikawaite, and cheralite) and Hf-rich zircon coexist. Magmatic (?) zircon contains numerous inclusions of rutile, fluorite, U -Th and REE minerals, such as uranothorite, cheralite, monazite, and xenotime.Composition variations in Ta / (Ta + Nb) and Mn / (Mn + Fe) in columbite range from 0.07-0.42 and 0.04-0.33, respectively, and Hf contents in zircon from 1.92-6.46 of the two mineralized shear zones reflect the extreme degree of magmatic fractionation. Flow samples of peralkalic granitic gneisses and cataclastic to mylonitic rocks from the southern shear zone have very low TiO2 (0.02 wt% -0.04 wt% ) With Sr [(15-20) × 10-6], and Ba [(47-78) × 10-6], with high Fe2O3T (0.94 wt% -1.99 wt%), CaO (0.14 wt% , Alkalis (9.2 wt% -10.1 wt%), Rb [(369-805) x 10-6], Zr [(1033-2261) x 10-6], Nb [(371-913) , Th [(36-110) × 10-6], Ta [(38-108) × 10-6], Pb [(39-364) × 10-6], Zn [(21-424) × 10-6], Y [(8-304) × 10-6], Hf[(29-157) × 10-6], and ΣREE [(64-304) × 10-6], especially HREE [(46-167) × 10-6] .Three samples from the northern shear zone also have very low TiO2 (0.03 wt%), Sr [(11-16) x 10-6], and Ba [(38-47) x 10-6], with high Fe2O3T (1.97 wt% -2.91 wt% (0.49 wt% -1.01 wt%), alkalis (7.2 wt% -8.3 wt%), Rb [(932-978) x 10-6], Zr [(1707-1953) x 10-6], Nb [ Ta [(100-112) × 10-6], U [(120-752) × 10-6], Th [(121-164) × 10-6], Pb [(260-2198) × 10-6], Zn [(483-1140) × 10-6], Y [(8-304) × 10-6], Hf [(67-106) × 10-6] , and ΣREE [(110-231) × 10-6], especially HREE [(91-177) × 10-6] .The very high Rb / Sr (57.5-88.9), and low Zr / Hf 25.6), Nb / Ta (7.7-9.8), and Th / U (0.21-1.01) are consistent with very frac-tioned fluorine-bearing granitic rocks that were altered and sheared. The field evidence, textural relations, and compositions of the ore minerals suggest that the main mineralizing event was magmatic (629 +/- 5 Ma, CHIME monazite) with later hydrothermal alteration and local remobilization of the high-field-strength elements.