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Discovery of a Tin-tungsten Mineralization in Northern Khartoum Province, Sudan

Published online by Cambridge University Press:  01 May 2009

D. C. Almond
D. C. Almond
Affiliation:
Dept. of Geology, University of Khartoum, Sudan.
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Abstract

A primary deposit of tin and tungsten has been discovered in association with granites of the Cambrian (?) sub-volcanic igneous complex at Sabaloka, on the Nile north of Khartoum. Wolfram and cassiterite occur in a stockwork of quartz veins which also contain minor amounts of sulphide minerals. The stockwork centres around a small intrusion of primary greisen lying on the contact of a porphyritic microgranite ring-dyke but the greisen and mineralizing solutions are believed to have originated from a nearby mass of biotite-muscovite granite. The deposit has many features in common with the primary tin veins associated with the Younger Granites of northern Nigeria and other parts of northern Africa.

Type
Articles
Information
Geological Magazine , Volume 104 , Issue 1 , February 1967 , pp. 1 - 12
Copyright
Copyright © Cambridge University Press 1967

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References

REFERENCES

Amin, M. S., 1947. A tin-tungsten deposit in Egypt. Econ. Geol., 42, 637–71.CrossRefGoogle Scholar
Burollet, P. F., 1963. Geological reconnaisance in the south-east of the Kufra basin. Compagnie des Petroles Total (Libye). Saharan Symposium, Tripoli (Libya), 1963.Google Scholar
de Kun, N., 1965. The mineral resources of Africa. Amsterdam, London and New York.Google Scholar
Delany, F. M., 1955. Ring structures in the northern Sudan. Ecl. geol. helv., 48, 133–48.Google Scholar
Delany, F. M., 1958. Observations on the Sabaloka Series of the Sudan. Trans. geol. Soc. S. Afr., 61, 111–24.Google Scholar
Falconer, J. D., 1921. The geology of the Plateau tin fields. Bull. geol. Surv. Nigeria, 1.Google Scholar
Hume, W. F., 1935. Geology of Egypt. Vol. II. Part II. The later plutonic and minor intrusive rocks. Cairo.Google Scholar
Jacobson, R. R. E., Macleod, W. N. and Black, R., 1958. Ring-complexes in the Younger Granite province of northern Nigeria. Mem. geol. Soc. Lond., 1.Google Scholar
Jacobson, R. R. E., Macleod, W. N. and Black, R., Snelling, N. J., and Truswell, J. F., 1963. Age determinations in the geology of Nigeria, with special reference to the Older and Younger Granites. Overseas Geol. min. Resour., 9, 168–82.Google Scholar
Mackay, R. A., Greenwood, R., and Rockingham, J. E., 1949. The geology of the Plateau tinfields—Resurvey 1945–48. Bull. geol. Surv. Nigeria, 19.Google Scholar
Mohr, P. A., 1962. The geology of Ethiopia. University College of Addis Ababa Press.Google Scholar
Said, R., 1962. The geology of Egypt. Amsterdam and London.Google Scholar