Greenstone Belt Clastic Sediment Continental Rift Banded Iron Formation Colluvial Deposit 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.


Unable to display preview. Download preview PDF.

Unable to display preview. Download preview PDF.

7 References

  1. Araujo, A. G., Perevalov, O. V., Guimaraes, F. R., Kondratiev, A. I., Tselikov, A. F., Khodirev, V. L., Polskoi, F. R., Agueev, Y. I., Voinovski, A. S., Sunda, P. & Joaquim, A. (1998): Carta de Recursos Minerais Mineral Resources Map, escala 1:1,000,000.-República de Angola, Instituto Geológico de Angola; Luanda.Google Scholar
  2. Carvalho, H. (1983): Notice explicative préliminaire sur la géologie de l’Angola.-Garica de Orta Sér. Géol. 6, 15–30; Lisboa.Google Scholar
  3. Duarte-morais, M.l., Castellano, M.c., Putignano, M.l. & Scrosso, I. (2004): The tectono-sedimentary evolution of the Kwanza Basin (Angola).-20th Colloquium Africa Geology, Abstr. Vol., 143; Orleans.Google Scholar
  4. Knoche, G. (1982): Angola — Rohstoffwissenschaftlicher Länderbericht 27, 1–84; Hannover.Google Scholar
  5. Minck, R., Ewins, N. P. & Pacavira, N. (2001): Sequence stratigraphy and hydrocarbon accumulations in the Miocene of Block 14, offshore Cabinda, Angola.-Africa Geoscience Review 8(1/2), 17/27; Paris.Google Scholar
  6. Porada, H. (1983): Geodynamic model for the geosynclinal development of the Damara orogen, Namibia/South West Africa.-In: H. Martin & F. W. Eder (eds.), Intracontinental fold belts, 503–542; Springer, Berlin.Google Scholar

Copyright information

© Springer-Verlag Berlin Heidelberg 2006

Personalised recommendations