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Soliman, M. M. (1981) Geochemical surveys for Sn, Nb, Cu and Au mineralization, Mueilha-Dungash area, Southeastern Desert, Egypt. Geological Magazine, 118 (5) 545-549 doi:10.1017/s001675680003291x

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Reference TypeJournal (article/letter/editorial)
TitleGeochemical surveys for Sn, Nb, Cu and Au mineralization, Mueilha-Dungash area, Southeastern Desert, Egypt
JournalGeological Magazine
AuthorsSoliman, M. M.Author
Year1981 (September)Volume118
Issue5
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s001675680003291xSearch in ResearchGate
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Mindat Ref. ID251990Long-form Identifiermindat:1:5:251990:0
GUID0
Full ReferenceSoliman, M. M. (1981) Geochemical surveys for Sn, Nb, Cu and Au mineralization, Mueilha-Dungash area, Southeastern Desert, Egypt. Geological Magazine, 118 (5) 545-549 doi:10.1017/s001675680003291x
Plain TextSoliman, M. M. (1981) Geochemical surveys for Sn, Nb, Cu and Au mineralization, Mueilha-Dungash area, Southeastern Desert, Egypt. Geological Magazine, 118 (5) 545-549 doi:10.1017/s001675680003291x
In(1981, September) Geological Magazine Vol. 118 (5) Cambridge University Press (CUP)
Abstract/NotesSummaryGeochemical stream sediments and bed-rock surveys were carried out on an area of about 400 km2 in the Muelha-Dungash area. Results indicated that Sn and Nb anomalies are concentrated near Gabal Mueilha and are related to the greisenized and albitized granites. Disseminated-type and vein-type gold mineralizations occur in propylitized granodiorites and quartz veins at Samut. Cu anomalies show wide distribution, with a large proportion confined to the central and southwestern parts of the district, where signs of hydrothermal alterations are clear. Most of the Cu, Sn and Nb anomalies coincide with ‘deep-seated tectonic zones’ having the direction of the Red Sea Rift System, which are characterized by anomalous radioactivity and intense metamorphism as well as metasomatism and mineralization caused by acidic intrusions. Under the arid conditions of the Southeastern Desert of Egypt, stream sediments and bed rock surveys proved to be suitable methods of prospecting.


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