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The Age of Some Carbonatite Igneous Activity in South-West Tanganyika

Published online by Cambridge University Press:  01 May 2009

J. A. Miller
Affiliation:
Department of Geodesy and Geophysics, Cambridge
P. E. Brown
Affiliation:
Department of Geology, Sheffield University

Abstract

Absolute age determinations by the potassium-argon method on biotite from the Musensi Hill intrusion and feldspar from a feldspathic breccia on the Mbeya Mountain Range indicate a Cretaceous age.

Type
Articles
Copyright
Copyright © Cambridge University Press 1963

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References

REFERENCES

Bailey, D. K., 1961. The Mid-Zambezi-Luangwa rift and related carbonatite activity. Geol. Mag., 98, 275284.CrossRefGoogle Scholar
Brown, P. E., 1962. The tectonic and metamorphic history of the Pre-cambrian rocks of the Mbeya region, south-west Tanganyika. Quart. J. Geol. Soc. Lond., 118, 295317.CrossRefGoogle Scholar
Fawley, A. P., and James., T. C., 1955. A pyrochlore carbonatite in southern Tanganyika. Econ. Geol., 50, 571585.CrossRefGoogle Scholar
Fick, L. J., and Van Der Heyde, C., 1959. Additional data on the geology of the Mbeya carbonatite. Econ. Geol., 54, 842872.CrossRefGoogle Scholar
Harkin, D. A., 1960. The Rungwe volcanics. Geol. Surv. Tanganyika, Mem. No. 2.Google Scholar