Correlations between U, Th Content and Metamorphic Grade in the Western Namaqualand Belt, South Africa, with Implications for Radioactive Heating of the Crust

Author:

ANDREOLI MARCO A. G.,HART RODGER J.,ASHWAL LEWIS D.,COETZEE HENK

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Reference111 articles.

1. Albat, H. M. (1984). The Proterozoic granulite-facies terrain around Kliprand, Namaqualand Metamorphic Complex. University of Cape Town, Bulletin of the Precambrian Research Unit33, 382.

2. Anders, E. & Grevesse, N. (1989). Abundances of the elements: meteoritic and solar. Geochimica et Cosmochimica Acta53, 197–214.

3. Andreoli, M. A. G. (1996). Progress Report: Summary of Geological Data for Vaalputs Boreholes HLD-2, -3, -4. Pretoria: Necsa, Unpublished Research Report GEA 1157, 16.

4. Andreoli, M. A. G. & Hart, R. J. (1990). Metasomatized granulites and eclogites of the Mozambique belt: implications for mantle devolatilization. In: Herbert, H. K. & Ho, S. E. (eds), Proceedings of the Conference on Stable Isotopes and Fluid Processes in Mineralization. Nedlands: University of Western Australia, Geology Department & Univ. Extension Publication 23, 121–140.

5. Andreoli, M. A. G., Andersen, N. J. B., Levin, M. & Niemand, N. (1986). Geology of the Vaalputs radioactive waste disposal site in the Republic of South Africa. In: Ainslie, L. C. (ed.) Proceedings of the Conference on the Treatment and Containment of Radioactive Waste, and its Disposal in Arid Environments. September 1986. Cape Town: Necsa, pp. 85–126.

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