Stream Sediments Geochemical Exploration in the Northwestern Part of Wadi Allaqi Area, South Eastern Desert, Egypt.

Geochemical stream sediments survey was conducted in the northwestern part of Wadi Allaqi area, Eastern Desert, Egypt. The area comprises Precambrian metasediments, intermediate metavolcanics, gabbro, and serpentinites, with intrusive masses of granites and quartz-porphyry and invaded by several quartz veins. The −1.0-mm size fraction is analyzed for As, Cu, S, Mo, Pb, Zn, Co, Ni, Rb, Ba, Sr, Nb, V, U, Th, Cr, Zr, La, Ce, Nd, and Y. The geochemical survey is supported by heavy minerals study in the −0.125 + 0.0625-mm fraction. The geochemical data were statistically investigated using Q-mode cluster and R-mode factor analyses as well as the enrichment factor. Factors 1 (Zr, Nb, Nd, La, and Y), 2 (V, Sr, and Zn), and 4 (Ba and Rb) are mainly controlled by the lithological characters of the rocks hosting Au-sulfide mineralizations and their accompanied hydrothermal alteration zones. In the mineralization Factor 3 (Cu, S, As, Ce, and Mo), arsenic, Cu, S, and Mo are direct indicators, while Ce is indirect one for the Au-sulfide mineralizations. The Cu-S-As-Mo association with Pb and Zn anomalies in the stream sediments draining the quartz-porphyry point to its porphyry copper mineralization. Cobalt and Ni (Factor 5) are pathfinders for the Fe- and Cu-sulfides, whereas Zn and Pb of Factor 8 are additional pathfinders for the Au-sulfide mineralizations. The southern stream sediments having high U/Th ratios with U-Mo association and draining granites traversed by pegmatites, as well as the stream sediments draining Um Garayat area and the quartz-porphyry stock with high abundance of monazite, zircon, epidote, sphene, and ilmenite, could signify sources of U and Th (Factor 7). Two watershed areas have distinct enrichment factors for arsenic suggesting unexplored extensions of Au-sulfide mineralization linked to the Allaqi shear-zone. The enrichment of the mineralization Factor 3 in the drainage system is mainly controlled by the prevailed mechanical dispersion for the hosting heavy minerals in such arid region with minor role of hydromorphic dispersion. The chemistry and mineralogy of the stream sediments are evidently allied to the drained bedrocks and their hosted mineralizations that signify a promising area for detailed exploration. [ABSTRACT FROM AUTHOR]