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The Junction Between the Mozambique and Zambesi Orogenic Belts; North-east Southern Rhodesia

Published online by Cambridge University Press:  01 May 2009

R. L. Johnson  and
J. R. Vail
R. L. Johnson
Affiliation:
Dept. of Mineral Resources, Regina, Saskatchewan.
J. R. Vail
Affiliation:
Research Institute of African Geology, The University of Leeds.
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Abstract

Reconnaissance work carried out in north-east Southern Rhodesia has shown that the Umkondo System, previously known in the Mozambique Belt, extends into the Zambesi Belt. It is further demonstrated that the two belts were broadly continuous in structure and metamorphism during the important orogeny c. 500 m·y. The possibility that the mobile belts were active considerably earlier than 500 m·y. is discussed.

Type
Articles
Information
Geological Magazine , Volume 102 , Issue 6 , December 1965 , pp. 489 - 495
Copyright
Copyright © Cambridge University Press 1965

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References

Clifford, T. N., 1963. The Damaran episode of tectono-thermal activity in South-West Africa, and its regional significance in Southern Africa. VIIth Ann. Rept. Leeds University Research Institute of African Geology for 1961–62, 37–42.Google Scholar
Holmes, A., and Cahen, L., 1955. African geochronology. Colon. Geol. Min. Resour., 5, 3–38.Google Scholar
Johnson, R. L., 1964. A preliminary account of craton-orogen relationships in north-east Southern Rhodesia. VIIIth Ann. Rept. Leeds University Research Institute of African Geology for 1962–63, 40–3.Google Scholar
MacGregor, A. M., 1951. Some milestones in the Pre-Cambrian of Southern Rhodesia. Trans, geol. Soc. S. Afr., 54, xxvii–lxxi.Google Scholar
McElhinny, M. W., and Opdyke, N. D., 1964. The palaeomagnetism of the Pre-Cambrian dolerites of eastern Southern Rhodesia, an example of geologic correlation by rock magnetism. J. geophys. Res., 69, 2465–2475.CrossRefGoogle Scholar
Snelling, N. J., Hamilton, E., Rex, D., Hornung, G. Johnson, R. L., Slater, D., and Vail, J. R., 1964. Age determinations from the Mozambique and Zambesi Orogenic Belts, central Africa. Nature, Lond., 201, 463–4.Google Scholar
Tyndale-Biscoe, R. M., 1958. The geology of a portion of the Inyanga district. Geol. Surv. S. Rhodesia Short Rept., No. 37, 11 pp.Google Scholar
Vail, J. R., in press. Aspects of the stratigraphy and structure of the Umkondo System in the Manica Belt of Southern Rhodesia and Mozambique, and an outline of the regional geology. Trans, geol. Soc. S. Afr., 67, pt. 2.Google Scholar
Vail, J. R., in press. The Umkondo System: Late Pre-Cambrian sedimentation along the western edge of the Mozambique Orogenic Belt in southern Africa. XXII Internal. Geol. Congr. India, Pt 12.Google Scholar